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    Predication methods of ultra-thin sandstone reservoirs and their application to blocks 14 and 17 in the Andes, Ecuador
    Guangfu WANG, Hai XU, Fayou LI, Jianfang SUN, Wenlong DUAN
    Oil & Gas Geology    2023, 44 (2): 247-263.   DOI: 10.11743/ogg20230201
    Abstract846)   HTML84)    PDF(pc) (12587KB)(355)       Save

    The minimum sand thickness for clastic reservoirs at medium burial depth between 2 500 and 3 500 meters to be predictable with current techniques is generally no more than 5 to 10 meters, while prediction of ultra-thin reservoirs with a thickness less than 5 meters remains a tough challenge. Based on the post-stack seismic data acquired and processed at different times from blocks 14 and 17 in the Andes of Ecuador, this study uses the post-stack consistent processing method driven by the structural trend surface to suppress and eliminate the interference of phase, energy, frequency and closure error on thin-bed reflection and reduce reservoir prediction uncertainty. The time-frequency attenuation, high-precision synthetic seismogram calibration method is employed to erase the accumulative time shift caused by formation absorption, accurately calibrate and analyse reflection characteristics of thin layers, and determine the minimum predominant frequency for resolving ultra-thin reservoirs. The weak reflection coefficient of thin layers is also effectively restored by using the high-resolution processing technology on post-stack broadband signals of “steady-state time-frequency-varying wavelet” without well data driving. The algorithm and workflow of facies-controlled waveform inversion are optimized based on broadband seismic waveform constraints. A series of technologies have then been developed and applied to the blocks, from which some tidal channel sand bodies of only 2 to 5 meters thick and 3 000 meters deep were successfully mapped. The drilling results of new appraisal wells and development wells verified that a prediction accuracy of at least 90 % with the methods has been reached.

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    Progresses and directions of unconventional natural gas exploration and development in the Carboniferous-Permian coal measure strata, Ordos Basin
    Xusheng Guo, Dehua Zhou, Peirong Zhao, Zengqin Liu, Dianwei Zhang, Dongjun Feng, Fengcun Xing, Wei Du, Gang Chen, Fan Yang, Chuanxiang Sun
    Oil & Gas Geology    2022, 43 (5): 1013-1023.   DOI: 10.11743/ogg20220501
    Abstract672)   HTML182)    PDF(pc) (4951KB)(430)       Save

    With the development and breakthroughs made in sweet spot assessment of unconventional gas, multi-stage hydraulic fracturing in horizontal wells, and simultaneous development of multiple pay zones, the exploration and development paradigm of unconventional gas has shifted from single mode to composite mode. The joint exploration and commingled production of unconventional gases from coal measure strata of marine-to-continental transitional facies is expected to become a new “unconventional revolution” following the shale revolution. The Carboniferous-Permian is of the most important source rock sequences in the Ordos Basin, featuring huge potential in unconventional gas resources, though at the initial stages of exploration and development. Based on exploration progresses made and research results achieved during the 13th Five-Year Plan period, we summarize the geological features of the Carboniferous-Permian coal-measure unconventional gas in the Ordos Basin, that is, “two sources, three highs, and three gases”. The Carboniferous-Permian is dominated by multiple types of lithology or lithological components, and the coal-rich components(“two sources”) are major targets in exploration,among others. The organic macerals of the source rocks are dominated by vitrinite, and organic pores and micro-fractures are the main reservoir spaces, characterized by high total organic carbon content, high thermal maturity, and high gas content (“three highs”). The gas occurrence is markedly differentiated between deep and shallow layers, with adsorbed gases dominating the shallow coal seams, and free gases occurring in the deep coal seams, resulting in the coexistence of coalbed methane, shale gas and tight sand gas (“three gases”), and the existence of their various combinations. Regarding challenges such as tightness of reservoirs, large difficulty in sweet spot identification, and relatively high stresses, we have developed drilling and completion technique of “long lateral, large pumping rate, large liquid volume and high sand load”, which could be of effective supports to breakthroughs made in unconventional gas exploration in deep coal-measure reservoirs. It is suggested to further strengthen the comprehensive research on coal-measure source rocks and lithological assemblages, establish theory and technology for integrated evaluation of geological and engineering sweet spots, and develop supporting technologies in exploration, development, and engineering, in an effort to accelerate high-quality development of unconventional gas in the Ordos Basin during the 14th Five-Year Plan period.

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    Progress and direction of geological modeling for deep and ultra-deep carbonate reservoirs
    Zhiliang HE, Xiangyuan ZHAO, Wenbiao ZHANG, Xinrui LYV, Dongya ZHU, Luanxiao ZHAO, Song HU, Wenbo ZHENG, Yanfeng LIU, Qian DING, Taizhong DUAN, Xiangyang HU, Jianfang SUN, Jianhua GENG
    Oil & Gas Geology    2023, 44 (1): 16-33.   DOI: 10.11743/ogg20230102
    Abstract560)   HTML50)    PDF(pc) (10794KB)(294)       Save

    Exploration and development of deep and ultra-deep carbonate reservoirs have been a hot and key research topic in the industry. Accurately depicting the spatial distribution and physical property parameters of the reservoirs has been a major challenge for an efficient oil and gas exploration and development. Based on an analysis of current development of reservoir geological analysis, logging evaluation, seismic prediction, geological modeling and other related technologies, this study is focused on figuring out the development mechanisms and distribution patterns of high-quality deep carbonate reservoirs by overcoming the data issues (scarcity, low quality and inaccuracy) and the high heterogeneity nature of the reservoir. A series of key technologies for characterization and modelling of the deep carbonate reservoirs have been developed, including technologies for construction of multi-scale and multi-attribute deep carbonate reservoir knowledge base; new technologies for geological analysis such as macroscopic to microscopic geological observation, in-situ micro-area qualitative and quantitative analysis for reservoir sedimentation and diagenetic environment, experiment and numerical simulation technologies for mechanism and process of reservoir development; new logging interpretation technologies, such as reservoir type identification and quantitative parameter evaluation based on global logging simulation, and sedimentary microfacies identification based on machine learning; new seismic prediction methods, such as seismic petrophysical modeling, machine learning technologies for rock physics guided reservoir parameter prediction and uncertainty evaluation; new geological modeling technologies such as new algorithm of multipoint geostatistics, geological process simulation, and geological modeling based on artificial intelligence. The technological processes of geological modeling of carbonate reservoirs under the control of karst unconformity, fault and sedimentary facies have been established respectively and applied to oil and gas reservoirs in Tahe, Shunbei and Yuanba blocks in the Tarim Basin and the Sichuan Basin, providing scientific basis for exploration and development deployment. The future research direction of geological modeling for deep and ultra-deep carbonate reservoirs is also predicted: updating geological knowledge base to support geological modeling; expanding the modeling technology based on geological process and improving its application; developing geophysical interpretation and prediction technologies based on artificial intelligence to improve the ability to depict complex reservoirs; developing new modeling methods based on artificial intelligence to continuously improve the accuracy of reservoir characterization and the reliability of models; and establishing rapid updating technology of geological models for deep reservoirs to continuously improve the efficiency and accuracy of model updating.

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    Tectono-sedimentary evolution, paleo-geographic reconstruction and play fairway delineation of the Lower Paleozoic, Ordos Basin
    Yan ZHOU, Siyi FU, Tao ZHANG, Hongde CHEN, Zhongtang SU, Juntao ZHANG, Chenggong ZHANG, Ziming LIU, Xiaoyu HAN
    Oil & Gas Geology    2023, 44 (2): 264-275.   DOI: 10.11743/ogg20230202
    Abstract445)   HTML75)    PDF(pc) (12140KB)(261)       Save

    The Lower Paleozoic has been an important target for natural gas exploration in the Ordos Basin. Several suites of gas-bearing sequences, such as weathering crust reservoir on top of the Ordovician, middle assemblage dolomite and sub-salt dolomite, have been discovered successively, which proves that the Lower Paleozoic in the basin is of good exploration and development potentials, and thus paleo-geographic reconstruction there is in urgent need. The study proposes a new idea of play fairway delineation of the Lower Paleozoic in the Ordos Basin from the perspective of tectono-sedimentary evolution and paleo-geographic reconstruction therein. The research shows that Ordos Basin experienced five stages of evolution, namely, the Archean-Proterozoic fault depression-deposition stage, the Cambrian-Ordovician deposition-denudation stage, the Carboniferous-Triassic stable depression-deposition stage, the Jurassic-Cretaceous compressional hydrocarbon accumulation stage and the adjustment and finalization stage from the Late Cretaceous till present. The paleo-geographic pattern of the Lower Paleozoic Ordos Basin underwent the stages of paleo-land reduction, sediment filling, margin rifting and the alternated uplift-depression during the Early Ordovician, which controlled the distribution of quality play fairways. Besides, the latest exploration achievements help us identify four types of quality play fairways in terms of source-reservoir assemblage, spatial distribution and major controlling factors, that is, hydrocarbon accumulation within dolomite of marginal tidal-flat facies, hydrocarbon accumulation within the Ordovician pre-salt layer of intra-platform mound shoal facies, hydrocarbon accumulation within dolomite and shale of marginal tidal-flat and intra-platform mound shoal facies in the west, hydrocarbon accumulation within dolomite of karstification and shoal facies. The play fairways of different types feature separate hydrocarbon play elements and major controlling factors, and thereby targeted exploration strategies are in need.

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    Sequence stratigraphy and source-to-sink system: Connections and distinctions
    Hongtao Zhu, Xiaomin Zhu, Qianghu Liu, Changgui Xu, Xiaofeng Du
    Oil & Gas Geology    2022, 43 (4): 763-776.   DOI: 10.11743/ogg20220403
    Abstract406)   HTML41)    PDF(pc) (7760KB)(292)       Save

    Both the sequence stratigraphy and source-to-sink system are modern geoscience disciplines with theories and methodologies being widely applied and employed. However, the connections and distinctions between the two have not been discussed thoroughly for a better discipline integration and synergy. The sequence stratigraphy is focused on establishing high-resolution isochronous stratigraphic frameworks for sinks and trying to reveal their sedimentary filling processes, temporal-spatial distribution patterns and genetic mechanisms. While the source-to-sink theory expands further to transport areas and provenances, tracing the dynamic responses of denudation, transport, and accumulation of sediments in multiple dimensions, and determining the driving mechanisms and prototype patterns of sediment partition from source to sink. The internal connections between the two disciplines are reflected mostly through the analysis of denudation-sedimentation response and quantitative prediction of sedimentary bodies in isochronous stratigraphic frameworks, while their distinctions are mainly illustrated during the description of different key elements and structures of inner sequence units. Judging by the current development trends, we could expect a rapid development of the methodology systems of the two disciplines in respects of standardization of their application, combination of ancient and modern data, and quantitative analyses and prediction through multi-disciplinary and multi-parameter integration.

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    Differences and main controlling factors of large-scale gas accumulations in typical giant carbonate gas fields: A case study on Anyue gas field in the Sichuan Basin and Jingbian gas field in the Ordos Basin
    Caineng ZOU, Zengye XIE, Jian LI, Lu ZHANG, Chunlong YANG, Huiying CUI, Xiaobo WANG, Zeqing GUO, Songqi PAN
    Oil & Gas Geology    2023, 44 (1): 1-15.   DOI: 10.11743/ogg20230101
    Abstract400)   HTML40)    PDF(pc) (4215KB)(313)       Save

    Anyue gas field in the Sichuan Basin and Jingbian gas field in the Ordos Basin are two giant marine carbonate gas fields with the largest overall scale and the largest single-layer scale respectively discovered in China so far. Based on the analysis of the source-location structure of gas reservoirs, the process of gas accumulation and the space-time configuration of key play elements during reservoir generation, we consider that Anyue and Jingbian gas fields are characterized by a variety of source-location structure types and source-trap configuration of high efficiency. However, Anyue gas field is of “in-situ” accumulation of pyrolysis gas from paleo-oil reservoirs in inherited paleo-uplift, while Jingbian gas field is of adjusted accumulation in the structural transformation zone of a slope. There are three key factors controlling the large-scale enrichment of Anyue and Jingbian gas fields. First, the hydrocarbon source rocks underwent abnormally thermal events, with the duration of thermal events with a heat flow value over 70 mW/m2 being about 70 Myr. Different types of kerogen got fully cracked to generate methane-dominated gases in large amount. Second, the multi-layered reservoirs of large scale and high quality are well developed due to the modification of favorable lithofacies by karstification. Third, many types of large-scale traps are well developed including structural, structural-lithologic, stratigraphic-lithologic and lithologic traps, being favorable for large-scale and effective accumulation of gas. The areas with ideal configuration relationship between high-energy beach body and lithologically tight zone within paleo-oil reservoirs or adjacent to hydrocarbon source rocks are favorable for discovering large-scale gas accumulation in the near future.

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    Review on provenance, transport-sedimentation dynamics and multi-source hydrocarbon sweet spots of continental fine-grained sedimentary rocks
    Zaixing Jiang, Yunzeng Wang, Li Wang, Xiangxin Kong, Yepeng Yang, Jianguo Zhang, Xinyu Xue
    Oil & Gas Geology    2022, 43 (5): 1039-1048.   DOI: 10.11743/ogg20220503
    Abstract396)   HTML41)    PDF(pc) (6474KB)(356)       Save

    With the rapid development of unconventional oil/gas industry, more and more attention has been paid to fine-grained sedimentary rocks. The study expounds the rock types, provenances, transport-sedimentation dynamics and hydrocarbon sweet spots of fine-grained sedimentary rocks of continental lacustrine facies in a systematic manner, based on the researches of fine-grained sedimentary rocks in recent years both at home and abroad. The accumulation of fine-grained sedimentary rocks in the continental lacustrine basin is mainly a result of multi-source supply of terrestrial, intrabasinal authigenic, volcanic and mixed-source sediments. The deposition mechanisms of fine-grained sediments include suspended sedimentation, gravity flow, volcanic, hydrothermal and intrabasinal biochemical activities, and the sediments may have undergone autochthonous re-deposition or re-deposition after short-distance transport before becoming consolidated rock. The provenance of fine-grained sediments plays a major role in determining the sedimentary characteristics, physical qualities, and hydrocarbon enrichment mechanism of the fine-grained sedimentary rocks. The study of provenance and transport-deposition dynamics of fine-grained sedimentary rocks is of great guiding value to shale oil/gas exploration and development.

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    Deep hydrothermalism of deep coarse-grained siliciclastic rocks and its geological significance: A case study of the 4th member of the Paleogene Shahejie Formation in Minfeng-Yanjia area, Dongying Sag, Bohai Bay Basin
    Jing Yuan, Tao Zhou, Jun Qiao, Guili Yang, Guanghao Zhao
    Oil & Gas Geology    2022, 43 (4): 929-942.   DOI: 10.11743/ogg20220415
    Abstract381)   HTML30)    PDF(pc) (8772KB)(145)       Save

    The deep coarse-grained siliciclastic rocks of the 4th member of the Paleogene Shahejie Formation (Es4) in Minfeng-Yanjia area of the eastern section of the steep slope zone to the north of Dongying Sag, Bohai Bay Basin, are taken to identify markers and time of deep hydrothermalism and make a preliminary discussion on its geological significance. A variety of data are applied in the study including the core, scanning electron microscopy (SEM), thin section, fluid inclusion, X-ray diffraction (XRD) of clay minerals, vitrinite reflectance (Ro), physical properties of core sample and hydrocarbon source Rock-Eval parameters; besides, the research results of tectonic evolution, magmatic activity, stratigraphic burial and hydrocarbon accumulation history are also taken into consideration. The results show that, there are explosive breccia, cubic pyrite and some mineral assemblages, such as mixed layer illite/montmorillonite-ankerite-apatite, mixed layer illite/montmorillonite-apatite-pyrite, chlorite-apatite-pyrite and apatite-pyrite, which just reflect the deep hydrothermalism in the Es4 coarse-grained siliciclastic rocks of the study area. The vertical evolution of clay minerals is characterized by an abnormal increase of illite/montmorillonite ratio and transient dramatic increase of kaolinite content. The contents of free hydrocarbon (S1) and pyrolysis hydrocarbon (S2) are abnormally high at a burial depth ranging from 3 400 m to 4 800 m, while they are relatively low at a burial depth of 5 500 m when the maximum pyrolysis temperature (Tmax) is abnormally high. At a burial depth of 4 269 m to 4 800 m, there are abnormally high-temperature inclusions in quartz fractures. The δ13 CCO2 in the carbon stable isotopes of natural gas is greater than -8 ‰, indicating inorganic origin and formation water of NaHCO3 type as associated with the deep CO2-rich hydrothermalism. The characteristics mentioned above all indicate deep fluid activity of mantle-derived CO2-rich origin in the Es4 coarse-grained siliciclastic rocks in Minfeng-Yanjia area during the Guantao-Minghuazhen sedimentary period. The deep hydrothermal fluid has played a dual role in reforming the physical properties of the coarse-grained siliciclastic reservoir. On the one hand, it causes fractures and promotes dissolution to improve the reservoir physical properties; on the other hand, the authigenic minerals in precipitation clog pores thereby hinder fluid migration and damage the physical properties of the reservoir. In addition, deep hydrothermal fluid has got involved in the thermal evolution and hydrocarbon generation of source rocks in the lower section of the 4th member of Shahejie Formation (Es4L), which has a potential impact on hydrocarbon expulsion and crude oil cracking of the source rocks.

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    Application of an integrated geology-reservoir engineering approach to shale oil development in Ansai area, Ordos Basin
    Chenglin Liu, Xinju Liu, Hongjun Zhang, Liyong Fan, Xiya Yang, Qibiao Zang, Bo Dai, Yue Meng, Hongliang Huo, Fang Wang
    Oil & Gas Geology    2022, 43 (5): 1238-1248.   DOI: 10.11743/ogg20220518
    Abstract375)   HTML18)    PDF(pc) (4806KB)(173)       Save

    Shale oil is a hot spot for petroleum exploration and development over the world. Given its unique geological features, enrichment mechanisms, and development conditions, shale oil is desirable for an integration of geology and reservoir engineering. A variety of technical methods such as field geological survey, core observation and sampling, logging data interpretation, geological and engineering parameter analysis and testing, are applied to geological evaluation of shale oil with focuses on reservoir lithology, thickness, porosity, permeability, oil saturation, fracture development and selection of sweet spots; while in terms of reservoir engineering evaluation, we propose a development method and parameters appropriate to the shale oil in Ansai area regarding the geological characteristics of sweet spots. The main understandings obtained are as follows. First, the 7th member of the Triassic Yanchang Formation (Chang 7 Member) in Ansai area, Ordos Basin is typical of continental shale oil mainly of delta front and semi-deep lacustrine subfacies. The tight sandstones therein mainly belong to reservoirs with low to ultra-low porosity and ultra-low permeability or non-reservoirs. In light of geological and geomechanical parameters, the reservoirs can be classified into 4 types from good to poor, including Type Ⅰ, Type Ⅱ, Type Ⅲ and Type Ⅳ, with the first two types being targets of sweet spots. Second, the flow of shale oil in reservoirs of the Chang 7 Member are driven by reservoir fluid, rocks'elastic expansion and gas dissolution, while the potential of energy supplement via gas injection is limited. For Type Ⅰ reservoirs selected by geological evaluation, the nine-point, seven-point or staggered horizontal well patterns are used for quasi-natural depletion, while the seven-point or five-point horizontal well patterns are used for development of Type Ⅱ reservoirs. Third, the typical horizontal wells in the Chang 7 Member is of low initial production with a high decline rate at the initial stage, but the decline rate gradually reduces in the later stages. Moreover, it features a long production cycle with a relatively stable production.

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    Oil & Gas Geology    2024, 45 (1): 309-.  
    Abstract367)      PDF(pc) (1076KB)(379)       Save
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    Application of an integrated geology-reservoir engineering approach to fracturing in unconventional gas reservoirs, Sichuan Basin and some insights
    Guangfu Wang, Fengxia Li, Haibo Wang, Jun Li, Hong Zhang, Tong Zhou, Xiaofei Shang, Linhua Pan, Yunqi Shen
    Oil & Gas Geology    2022, 43 (5): 1221-1237.   DOI: 10.11743/ogg20220517
    Abstract361)   HTML34)    PDF(pc) (10929KB)(232)       Save

    The concept of engineering integrated with geology originated and prevailing in North America has also been accepted and put into practice during the exploration and development of unconventional oil and gas in the rest of the world. It runs through the whole process that starts with well design, drilling and completion, and ends with fracturing and production, only with focus shifting along the way in adaptation to different geological conditions and exploration or development stages. The introduction of the integrated geology-reservoir engineering approach to fracturing in the Fuling shale gas field in Sichuan Basin has been quite fruitful except for some restrictions frequently felt during exploration activities in some frontier blocks. Due to the diversity and complexity of sedimentary and tectonics in the Sichuan Basin, exploratory/appraisal wells after fracturing are tested with greatly varying results (mostly with low gas flow) even if they are located in the same block or arranged closely to one another. This might be explained by an insufficient accuracy of 3D quantitative characterization and models for key geological engineering parameters such as fractures and in-situ stress in sweet spots, and a lack of adaptive quantitative simulation technologies such as optimal fracturing stage/cluster division, fracture geometry optimization and fracturing process control. This paper systematically summarizes the experiences of an integrated geological-reservoir engineering team gained during fracturing practice in exploratory and appraisal wells for tight gas and shale gas in the Sichuan basin. Their work includes a 3D geo-engineering model of regional unconventional gas reservoirs built with key parameters of geology and engineering such as spatial reservoir distribution, physical properties, gas content, rock mechanics, in-situ stress field, initial formation pressure, mineral contents and natural fractures based on multi-discipline collaboration of geology, well-logging, seismic survey and engineering. Furthermore, the team carried out a fracture propagation simulation based on the model and formed a specific integrative technology series and workflow that could enhance SRV and single well production through tracing and optimization of perforation and diversion parameters, fracturing fluid and proppant volume as well as pumping rate. The implementation of the approach in developing tight gas from the Qianfoya Formation, Puguang Gas field and shale gas from Lintanchang Block in the basin has been proven successful, thus providing a reference for the development of similar unconventional reservoirs.

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    Classification of lacustrine shale oil reservoirs in China and its significance
    Zhijun JIN, Qian ZHANG, Rukai ZHU, Lin DONG, Jinhua FU, Huimin LIU, Lu YUN, Guoyong LIU, Maowen LI, Xianzheng ZHAO, Xiaojun WANG, Suyun HU, Yong TANG, Zhenrui BAI, Dongsheng SUN, Xiaoguang LI
    Oil & Gas Geology    2023, 44 (4): 801-819.   DOI: 10.11743/ogg20230401
    Abstract358)   HTML44)    PDF(pc) (3874KB)(509)       Save

    China has significant potential for the exploration of lacustrine shale oil, which serves as an important alternative resource for conventional oil and gas. However, the development and recovery of lacustrine shale oil face significant constraints due to the lack of fundamental research, unclear mechanisms of its formation and accumulation, and the absence of standardized criteria for evaluating “sweet spots”. To address these issues, the authors proposed a set of simplified standards for lacustrine shale oil classification, taking into account previous research and the practical conditions of exploration and development. Based on the storage space and type of reservoir rocks, shale oil reservoirs are commonly classified into three major types, namely interbedded sand-shale, fractured shale, and pure shale, with the last type being taken as the focus of discussion in this paper. The pure shale type can be classified into laminated, bedded and massive shale oil reservoirs based on the sedimentary structure. Although the grain size was not taken as one of the parameters for shale oil classification, we kept the traditional three terminal element category and mixed category of minerals, and removed further subdivided subcategories; the Rock-Eval S1 was used instead of TOC and Ro to divide shale oil reservoirs into three types: low oil content, medium oil content and high oil content; the formation pressure coefficient less than 0.8 is defined as abnormally low pressure, 0.8 ~ 1.2 is classified as normal pressure, and greater than 1.2 is classified as abnormally high pressure; the crude oil viscosity is not involved in the classification of shale oil reservoir types. In addition, this study designated type Ⅰ, Ⅱ and Ⅲ sweet spots, and discussed the representative types of shale oil reservoirs in typical continental basins in China. This paper enhances our understanding of the assessment standards, the type of rocks and the distribution of “sweet spots” in shale oil reservoirs. As a result, this research contributes to the advancement of shale oil exploration and development, providing valuable insights for future endeavors in this field.

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    Factors controlling lacustrine shale oil adsorption in the Jiyang Depression, Bohai Bay Basin
    Yongshi Wang, Zheng Li, Min Wang, Youshu Bao, Rifang Zhu, Jun Liu, Lianbo Wu, Limin Yu
    Oil & Gas Geology    2022, 43 (3): 489-498.   DOI: 10.11743/ogg20220301
    Abstract356)   HTML29)    PDF(pc) (2347KB)(348)       Save

    It is of great significance to determining the amount of adsorbed oil and its control factors for the evaluation of shale oil resources and prediction of play fairway in shale oil exploration. The Shahejie shale in the Jiyang Depression is taken to determine the quantity of adsorbed shale oil by improved pyrolysis experiments. Meanwhile, the study reveals the factors influencing shale oil adsorption volume such as shale physical properties, shale compositions, shale oil components, as well as maturity of organic matters, temperature and pressure, etc., by an integration of molecular simulation technology, micro-adsorption mechanism and macro-experimental data. The results show that shale oil reservoirs featuring large pore volume, high TOC content, low saturated hydrocarbon content, low maturity, and low temperature, are of higher oil adsorption capacity, and TOC content and organic matter maturity are the main factors controlling oil adsorption of lacustrine shale oil reservoirs with low maturity.

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    Logging evaluation of “double sweet spot” in shale gas reservoirs
    Shuanglian Liu
    Oil & Gas Geology    2022, 43 (4): 1005-1012.   DOI: 10.11743/ogg20220420
    Abstract349)   HTML19)    PDF(pc) (3523KB)(202)       Save

    Evaluation of “double sweet spot” in shale gas reservoirs, i.e. shale gas sweet spot that are both geologically and engineeringly feasible, is challenging due to insufficient accuracy of gas saturation calculation, limitations of fracability assessment methods (though quite a few), and inadequate integration between the geological and engineering assessments. In view of these, a gas abundance curve representing the geological “sweet spot” is established to tackle the accuracy problem through a sequential reconstruction of the sensitivity relationship between logging curves and gas bearing property based on gas bearing principles. A comprehensive fracability index representing the engineering “sweet spot” is developed to enhance the usability of the fracability assessment methods based on the correlation of rock brittleness index, mechanic parameters and in-situ stress difference coefficients to fracturing. And a geology-engineering evaluation chart is also proposed to better integrate the two aspects based on the production data and productivity classification of layers tested. This study improves the accuracy of qualitative identification and fracability assessment of shale gas sweet spots. The chart has been proven to be effective in recognizing high- medium- and low-potential gas pay zones as well as dry layers. Practices show that the technology is applicable and reliable in assessing shallow/deep layers in the Sichuan Basin and its periphery.

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    Lithofacies palaeogeographic evolution and sedimentary model of the Ordovician in the Tarim Basin
    Herong Zheng, Jingchun Tian, Zongquan Hu, Xiang Zhang, Yongqiang Zhao, Wanbin Meng
    Oil & Gas Geology    2022, 43 (4): 733-745.   DOI: 10.11743/ogg20220401
    Abstract347)   HTML44)    PDF(pc) (10322KB)(284)       Save

    Upon previous researches, insights have been gained through detailed observation of 12 new outcrop sections and cores (mostly gathered after 2016) from 31 typical wells on the perihhery of Tarim Basin as well as fine interpretation of sedimentary facies in 82 wells together with the interpretation and seismic facies identification from 188 two-dimensional seismic lines and three-dimensional seismic data in five acreages focusing on the Ordovician in the Tarim Basin. Firstly, sedimentary facies types and features are determined by observing single outcrop sections and analyzing drilling data of single wells. Secondly, sedimentary facies changes are mapped through correlation between outcrop sections and well profiles. Thirdly, facies boundaries are delineated based on seismic facies types and their planar distribution determined through seismic interpretation and tracing. Finally, the lithofacies paleogeography during the deposition of each formation of the Ordovician are mapped to reveal their paleogeographic and sedimentary patterns. The results show that the sedimentary period of the Penglaiba-Yijianfang Formations in the early Ordovician is rather a pattern of "one platform with two edges and two basins" than a pattern of "a west platform coupled with an east basin" that as previously determined. The Ordovician carbonate platform is suggested to have evolved from a unified carbonate platform to multiple platforms after differentiation and to the final extinction. Based on these understandings, three sedimentary filling models are established for the evolution of the Ordovician, i.e., the early single platform - coexisting gentle slope and steep slope edge - basin, the middle multiplatform - multiple edge - multiple basin and the late marine environment with terrigenous clastic input.

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    Predictive stratigraphy: From sequence stratigraphy to source-to-sink system
    Changgui XU, Chenglin GONG
    Oil & Gas Geology    2023, 44 (3): 521-538.   DOI: 10.11743/ogg20230301
    Abstract340)   HTML44)    PDF(pc) (9454KB)(384)       Save

    Predictive stratigraphy with the ability to predict sedimentary fills and high-quality reservoirs has been widely applied to basin analysis and hydrocarbon exploration, and has undergone the evolutionary process from sequence stratigraphy to source-to-sink system for reservoir quality prediction. In response to the challenge of predicting favorable play elements (i.e. reservoir and seal), geologists of ExxonMobil established the sequence stratigraphic methodology and theory. To answer why the sequences do not necessarily control sandstone development and lowstand systems tract does not necessarily result in fan deposits, the geologists adopted the source-to-sink hypothesis in predicting high-quality reservoirs, creating the source-to-sink-based sandstone mapping methodology. The present study reviews the status quo of sequence stratigraphy and major advances in application to marine and lacustrine sequences, and introduces major progress in the application of source-to-sink-based methodology to predict high-quality reservoirs in both continental-marine and continental-lacustrine systems. A source-channel-sink-diagenesis coupling technique to predict high-quality reservoirs is proposed in the study to solve the difficulty encountered in exploring why the source-to-sink system serves to control sandstone development, but not necessarily determine reservoir formation.

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    Key factors and directions of exploration in the Cambrian pre-salt sequence, Tarim Basin
    Haitao Lyu, Feng Geng, Kai Shang
    Oil & Gas Geology    2022, 43 (5): 1049-1058.   DOI: 10.11743/ogg20220504
    Abstract333)   HTML25)    PDF(pc) (4914KB)(312)       Save

    The Cambrian pre-salt sequence has been an important strategic successor play for oil and gas exploration with the greatest exploration potential in the Tarim Basin. However, no significant discoveries have been made for the past many years, with some key problems yet to be solved. Based on the summary and review of the achievements of key exploration wells in the Cambrian in the Tarim Basin, the conditions of hydrocarbon accumulation in the Cambrian pre-salt sequence are recognized, while pointing out the play fairways for exploration and the directions for research in the near future. The study shows that the Cambrian pre-salt sequence in the Tarim Basin is of better geological conditions for hydrocarbon accumulation such as source rocks, reservoirs and cap rocks, but there are differences in the configuration of play elements in different zones. Generally speaking, there are two hydrocarbon accumulation patterns in the pre-salt sequence, namely the “accumulation via vertical migration of hydrocarbons from indigenous source rocks” and the “accumulation via lateral migration of hydrocarbons from allochthonous source rocks”. It is pointed out that the Tazhong Uplift facing Manjiaer Sag, the Selibuya-Haimiluosi-Mazhatage structural belt facing Maigaiti Slope and the Akekule Salient of Tabei Uplift are the key areas for further exploration, and the key research directions are put forward respectively.

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    Has the Ordos Block, a cratonic block been reactivated?
    Dengfa He, Hongping Bao, Baize Kai, Yanhua Xu, Renqi Lu, Caili Zhang, Liubing Wei, Xiang Cheng
    Oil & Gas Geology    2022, 43 (6): 1271-1291.   DOI: 10.11743/ogg20220601
    Abstract331)   HTML43)    PDF(pc) (6638KB)(299)       Save

    The activity of a cratonic block during its evolution is the key in studying the continental preservation. Cratonic block reactivation of diverse scales is in close relation to mineral deposits such as oil, gas, coal, uranium and salt, and controls the intra-plate earthquake activity, thus has been one of the hot topics in the field of energy, resource, and environment researches. The Ordos Block located in western North-China craton (NCC), is taken to reveal its tectonic activities, referring to as “reactivation” in the study. The analysis of deep boreholes and high-resolution reflection seismic profiles, indicates that the reactivation of the Ordos Block can be shown in six aspects as follows. First, five stages of rifting or extension in or around the block occurred during the Mesoproterozoic, the Cambrian to Early Ordovician, the Carboniferous to Early Permian, the Middle to Late Triassic, and the Cenozoic; second, there were six stages of magmatism in the block during the Middle to Late Proterozoic, the Ordovician, the Late Carboniferous, the Middle to Late Triassic, the Early Cretaceous, and the Late Miocene to Quaternary, with the magmatic events coming to peak during the Changchengnian Period and the Early Cretaceous; third, there were seven stages of faulting and development of faulting-related folds; fourth, there are ten regional unconformities developed including the Ch/AnCh, Jx/AnJx, Z/AnZ, C?/AnC?, O/AnO, C/AnC, T/AnT, J/AnJ, K/AnK, and Q/AnQ; fifth, the block underwent four tectonic subsidence cycles of the Middle to Late Proterozoic, the Early Paleozoic, the Carboniferous to the Triassic, and the Jurassic to Cretaceous, with a marked migration of the subsiding centers; and sixth, a number of strong earthquakes occurred along the peripheries and the interior of the Ordos Block with the interior uplifting while the periphery rifting and rapidly subsiding during the Cenozoic. The evolution of the Ordos Block is predominantly controlled by the adjoining plate tectonics and the deep tectonic activities, to some extent with a possible large-scale thinning of the lithosphere in the Early Cretaceous, and also the reactivation and thinning of the lithosphere in northern part of the Ordos Block during the Late Cenozoic, which is resulted from the anti-clockwise rotation of the block, and thus the upward intrusion of the partial molten melts of the upper mantle along the weak zones of the graben systems around. The Ordos Block therefore took typical properties of reactivation, which may have played a profound role in the basin formation, the hydrocarbon generation, and the pool-formation in the block.

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    Sequence stratigraphy and lithofacies characteristics of fine-grained deposits of Wufeng-Longmaxi Formations in the Sichuan Basin and on its periphery
    Zongquan Hu, Wei Du, Tong Zhu, Zengqin Liu
    Oil & Gas Geology    2022, 43 (5): 1024-1038.   DOI: 10.11743/ogg20220502
    Abstract321)   HTML38)    PDF(pc) (10788KB)(250)       Save

    This paper takes the shale samples from the Wufeng Formation and the first member of Longmaxi Formation in the Sichuan Basin and its periphery as the research subject. Through the comparative analysis of drilling data, core and outcrop analysis, and test data, a study on the sequence stratigraphic division and correlation, lithofacies classification and identification, and sedimentary microfacies-lithofacies distribution of the rocks is carried out. The results show that the fine-grained deposits of study interval can be divided into three third-order sequences (SQ1, SQ2, and SQ3), which are subdivided into seven systems tracts. High-quality shales are mainly distributed in the transgressive systems tracts (TST) of the three sequences, of which high-quality shales of SQ2-TST are the most widely distributed. The lithofacies are mainly organic siliceous shale, organic-rich limy siliceous shale, and medium-high organic siliceous argillaceous shale. The regional distribution of different types of inorganic minerals is clarified. The contents of carbonate minerals are relatively high near the central Sichuan paleo-high and northern Guizhou Uplift. With the increase of water depth, the contents of clay minerals and quartz minerals gradually increase. The sedimentary-lithofacies of SQ2-TST is mapped by using the contour maps of the content of three terminal principal minerals (quartz, clay, and carbonate) and the content of total organic carbon (TOC), in combination with the contour maps of parameters such as geochemical parameters (Th/U) and isopachous maps. On the periphery of the central Sichuan paleo-high, central northern Guizhou paleo-high, and northern Sichuan paleo-high, medium-low organic argillaceous shales and medium-low organic limy siliceous argillaceous shales deposited. In the deep-water shelf of southern Sichuan Basin enclosed by the central Sichuan paleo-high and central northern Guizhou paleo-high, organic-rich limy siliceous argillaceous shales are mainly deposited. organic-rich siliceous shales are mainly developed in the Fuling area extending to the northeast of the Sichuan Basin.

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    Development of the Upper Permian Wujiaping shale in Hongxing area, eastern Sichuan Basin, and its significance to shale gas enrichment
    Pengwei Wang, Zhongbao Liu, Xiong Li, Haotian Liu, Lin Zhou, Xiong Xiao, Ruyue Wang, Peng Li
    Oil & Gas Geology    2022, 43 (5): 1102-1114.   DOI: 10.11743/ogg20220508
    Abstract316)   HTML16)    PDF(pc) (14188KB)(177)       Save

    The Wujiaping marine shale of the Upper Permian in the eastern Sichuan Basin is an important successor for shale gas exploration in the Sichuan Basin, where shale gas enrichment conditions and favorable exploration intervals are yet to be clarified. The study investigates source rocks and reservoir quality of the Wujiaping shale in Well HY 1 and their changes in vertical via petrology and geochemistry analysis, reservoir description and characterization as well as gas-bearing potential test, and the exploration prospects are thereby identified. Results show that the organic-rich shale is developed in the first sub-member of the first member of the Wujiaping Formation (Wu11) of tidal flat-lagoon facies and the second member (Wu2) of deep shelf facies. To be specific, the Wu11 is dominated by argillaceous shale, Wu21 bymixed siliceous shale and siliceous shale, and the Wu22 by siliceous shale and calcareous shale. Compared with the argillaceous shale in the Wu11, the mixed siliceous and siliceous shale in the Wu2 is characterized by high brittle mineral content (63.2 %), high organic matter abundance (TOC = 8.87 %), favorable organic matters (Type Ⅱ1), well-developed organic pores, and good physical properties (a porosity of 5.59 %). Among others, the source rock quality and reservoir capacity of the Wu21 are better than those of the Wu22. It can be concluded that the organic-rich shale of the Wu21 is favorable for shale gas exploration in the study area.

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    Wettability of the Permian Fengcheng Formation shale in the Mahu Sag, Junggar Basin, and its main control factors
    Guowei Zheng, Zhiye Gao, Liliang Huang, Zhenxue Jiang, Wenjun He, Jiaqi Chang, Longfei Duan, Weihang Wei, Zhiwei Wang
    Oil & Gas Geology    2022, 43 (5): 1206-1220.   DOI: 10.11743/ogg20220516
    Abstract316)   HTML11)    PDF(pc) (5511KB)(148)       Save

    Shale wettability is of great significance to relative permeability and capillary force of a reservoir, ultimately affecting the hydrocarbon accumulation process in shale as well as the shale oil/gas recovery rate. This study focuses on the wettability characteristics and main control factors of the Permian Fengcheng Formation shale in the Mahu Sag, Junggar Basin, by means of contact angle measurement and spontaneous imbibition plus micro-CT experiment. The results are shown as follows. First, the Fengcheng Formation shale in the Mahu Sag is of generally mixed wettability while prone to oil-wet, and the affinity of different lithofacies to water is listed out from the top, that is, felsic shale, limy felsic shale, dolomitic felsic shale, felsic dolomitic shale, and siltstone. Second, the shale wettability is jointly controlled by multiple factors including organic matter abundance, mineral composition, and pore structure. The shale hydrophobicity is positively correlated with the TOC, dolomite content, negatively with the quartz content, and in staged correlation with the calcite content; the larger the pore volume occupied by macro-pores, the more oil-wet is the shale sample. Third, the connectivity of oil-wet pores tends to grow better along the direction of crack and lamina development. A pore system of clustered type and certain connectivity is prone to form in dolomitic glomerates, which can form an unique shale oil storage space and migration pathway together with the interconnected small pores in the shale matrix. Fourth, the pores less than 1 μm have better connectivity and act as the main migration pathways for shale oil, while those larger than 1 μm with poor connectivity serve as the main storage space for shale oil. Fifth, it is preliminarily concluded that the high-quality shale oil reservoirs are of siltstone and dolomitic felsic shale with well-developed cracks, dolomitic glomerates and laminar structures in the study area according to the wettability characteristics of different lithofacies and sedimentary structure characteristics.

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    Reservoir exploration of the Permian Maokou Formation in the Sichuan Basin and enlightenment obtained
    Yu Zhang, Qinggu Cao, Kaiping Luo, Longlong Li, Jinlian Liu
    Oil & Gas Geology    2022, 43 (3): 610-620.   DOI: 10.11743/ogg20220310
    Abstract315)   HTML23)    PDF(pc) (4963KB)(223)       Save

    The Permian Maokou Formation among the first batch of exploration targets is one of the most actively explored formations in the Sichuan Basin. Gas reservoirs in the formation can be classified into five types in terms of reservoir characteristics, that is, reservoirs of fracture type, karst fractured-vuggy type, hydrothermal dolomite type, shoal dolomite type and marl type, and are dominated by lithologic reservoirs. These types of gas reservoirs show diverse characters in different stratigraphic intervals and different plays. The previous exploration results of Maokou Formation and characteristics of different gas reservoirs, demonstrate that favorable sedimentary facies zones such as marginal-platform shoals, intra-platform shoals and deep gentle slopes serve as basic conditions for reservoir development, and pseudocontemporaneous dolomitization, late hydrothermal dolomitization, epigenetic karstification, and tectonic transformations such as folds and faults are the keys to forming high-quality reservoirs therein. It is pointed out that karst fractured-vuggy reservoirs, dolomite reservoirs of shoal facies and marl reservoirs in the first member of Maokou Formation (Mao 1 Member) as controlled by facies (geomorphology), characterized by continuous distribution and high quality, are the main exploration targets in the future. The northeastern and southern-southeastern parts of Sichuan Basin are the most favorable play fairways for the exploration of Maokou Formation. The superposition of various reservoir types and exploration fields is of value to setting up a holistic pattern for exploration.

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    Simulation of dynamic fracture network in fractured horizontal well for unconventional reservoirs: Theory and application
    Chuanxi Liu, Wenchao Fang, Xuejie Qin
    Oil & Gas Geology    2022, 43 (3): 696-702.   DOI: 10.11743/ogg20220317
    Abstract314)   HTML13)    PDF(pc) (2617KB)(168)       Save

    When a fractured horizontal well in unconventional reservoirs is brought online, change in reservoir pressure may lead to fracture deformation, resulting in the formation of dynamic fracture network that greatly affects well productivity. To simulate the effect of dynamic fracture network on the development of unconventional reservoirs and improve the designation level of development strategy, the study builds a mathematical model to characterize the time variant and the heterogeneous distribution of fracture width, which can simultaneously simulate the changes of fracture width and fracture length in a reservoir. Then, the conductivity modification technique is adopted to couple the fracture deformation model with discrete fracture simulation model. A reservoir numerical simulator that can model dynamic fracture network is then developed. Finally, the simulator is applied to the simulation of a typical reservoir model and an actual fractured horizontal well model, respectively. Dynamic fracture network models for different production periods are thereby obtained, and the effect of dynamic fracture network on the well productivity is clarified. In all, the simulation results indicate that the simulated performance is in better agreement with practical well performance when the fracture deformation is considered in the simulator.

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    Deep learning-based geological modeling driven by sedimentary process simulation
    Yanfeng LIU, Taizhong DUAN, Yuan HUANG, Wenbiao ZHANG, Meng LI
    Oil & Gas Geology    2023, 44 (1): 226-237.   DOI: 10.11743/ogg20230119
    Abstract312)   HTML16)    PDF(pc) (3120KB)(208)       Save

    Problems including insufficient quantity and low resolution of data face exploration and development of deep and complex reservoir targets, and the traditional geological modeling methods have been inadequate in terms of technical needs. The intelligent geological modeling represented by deep learning capable of fully integrating multi-scale and multi-dimensional data as well as expert knowledge, is a key research and development direction of geological modeling technology. The study discusses the deep learning-based geological modeling driven by sedimentary process simulation following the comprehensive analysis of the advantages and disadvantages of stratigraphic forward modeling and deep learning-based geological modeling technology. First, forward modeling of sedimentation is carried out based on comprehensive geological analysis, parameter uncertainty is analyzed, and a large amount of geological models are established through parameter disturbance as a training dataset; Second, the geological patterns contained in the learning dataset are learned with the conditional Generative Adversarial Nets (cGAN), in which the Generative Adversarial Networks (GAN) takes the conditional data such as well and seismic data as the input, and the geological model as the output; Finally, the trained GAN is applied to the real conditional data to obtain the geological model of the target block. The feasibility of this method is verified through testing on the typical geological profiles of the main block of Puguang gas reservoir, and the impact of the training dataset scale on simulation results is analyzed. The combination of sedimentary simulation and deep learning could make up for the shortage of training data and indirectly realize knowledge-driven deep learning-based geological modeling. The method is therefore of great significance to popularization.

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    Research procedure of astrostratigraphy and case study of Dongying Sag, Bohai Bay Basin
    Jun Peng, Ledan Yu, Tianyu Xu, Haodong Han, Yiming Yang
    Oil & Gas Geology    2022, 43 (6): 1292-1308.   DOI: 10.11743/ogg20220602
    Abstract311)   HTML25)    PDF(pc) (2081KB)(202)       Save

    Astrostratigraphy is to study the sedimentary sequence formed by the periodic changes of the Earth's orbit based on the Milankovitch cycle theory. It has been developing rapidly since its inception and is widely applied. However, the application of indicators and methods of data processing have always been the focus and difficulty in cycle stratigraphy research. Based on the division of astronomical cycles in the third and fourth members of Shahejie Formation in the Dongying Sag (Es3 and Es4), as well as research results gained from both home and abroad, we know that the alternative parameters of sedimentary stratigraphic sequences in astrostratigraphy research at present include paleontological parameters, geophysical and geochemical parameters, etc. The astronomical cycle identification methods mainly include lithology-based visual identification and time series analysis. While the orbital period ratio method, astronomical modulation method and hypothesis testing method are for checking and tuning the results of cyclotrons. The issues in need of attention in the current astronomical cycle stratigraphic research mainly include: the comprehensive application of alternative indicators of sedimentary stratigraphic sequences, the optimization of multiple time-frequency analysis methods, the calibration of cycle division results, and the establishment of astronomical age scales. In this study, a relatively systematic set of astronomical cycle division schemes is sorted out including the selection of alternative indicators of depositional sequences, the optimization of time series analysis methods, and the verification of cycle results. It will be of value to studying the sub-Milankovitch cycle with fine subdivision of the stratum to the millennium and 10,000-year-old level, and of referential value for researchers interested in astronomical age scales, facilitating the development of astrostratigraphy.

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    Deep learning-based geological modeling of ultra-deep fault-karst reservoirs in Shunbei oilfield, Tarim Basin
    Taizhong DUAN, Wenbiao ZHANG, Zhiliang HE, Yanfeng LIU, Qiqi MA, Meng LI, Peiqing LIAN, Yuan HUANG
    Oil & Gas Geology    2023, 44 (1): 203-212.   DOI: 10.11743/ogg20230117
    Abstract304)   HTML23)    PDF(pc) (3888KB)(211)       Save

    Fault-karst reservoir is of a special type distributed in the Ordovician strata in the Tarim Basin, China. It’s characterized by deep burial, complex genesis and strong heterogeneity. Due to sparse well data and low seismic quality and other adverse conditions, its accurate characterization and fine modeling are faced with great challenges. In the study, an integration of drilling, core, outcrop and 3D seismic data is applied to build a deep learning-based training dataset for the fault-karst reservoir with the guidance of architecture mode of fault-controlled fractured-vuggy reservoir. Based on the comprehensive analysis of deep learning network, we propose a deep learning-based modeling method suitable for fault-karst reservoirs. The results show that the “in-situ, equal-scale” training dataset established based on multi-source data is the basis for deep learning-based modeling of fault-karst reservoirs. The selected pix 2 pix (P2P) neural network could realize the 3D model prediction of fault-karst reservoirs by seismic data. A 3D fault-karst reservoir model is then established for the south segment of the No. 5 fault zone in Shunbei area following the built of training network. The model is conformed to the geological mode and distribution pattern of the reservoir type on all fronts, and also highly consistent with the reservoir prediction based on drilling data. One of the key research directions therefore lies in improving the accuracy and conditional degree of deep learning-based geological modeling of fault-karst reservoirs.

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    Mechanisms for lacustrine shale oil enrichment in Chinese sedimentary basins
    Xusheng GUO, Xiaoxiao MA, Maowen LI, Menhui QIAN, Zongquan HU
    Oil & Gas Geology    2023, 44 (6): 1333-1349.   DOI: 10.11743/ogg20230601
    Abstract302)   HTML29)    PDF(pc) (4379KB)(545)       Save

    By analyzing the tectonic and sedimentary environments for the formation of organic-rich shales in China’s continental lacustrine basins, we identify significant differences in the development of high-quality continental source rocks across various types of lacustrine basins. For shale sequences deposited in fresh-water lacustrine basins, the main lithofacies are felsic and clayey shales, as observed from the 1st member of the Upper Cretaceous Qingshankou Formation (K2qn1 section) in the Songliao Basin and the 7th member of the Triassic Yanchang Formation (T3yc7 section) in the Ordos Basin. For shale sequences developed in a saline lacustrine environment, however, carbonates and evaporites are dominant lithofacies, as represented by the Paleogene Shahejie Formation in the Jiyang Depression. There are three types of lithofacies assemblages for Chinese lacustrine shales, that is, the shale interbedded/intercalated with sand, mixed shale, and clayey shale. These lithofacies assemblages determine the hydrocarbon source-reservoir coupling characteristics, differential evolution of hydrocarbon generation, and property differences of in-situ fluids in the lacustrine organic-rich shales. The shale interbedded/intercalated with sand assemblage is characterized by source-reservoir separation and near-source migration. The mixed shale assemblage shows macroscopic integration and microscopic separation between source rock and reservoir. In contrast, the clayey shale acts as both the source and reservoir of in-situ generated hydrocarbons, featuring pervasive oil distribution. As revealed by evidence, inorganic pores provide the most favorable storage space for lacustrine shale oil in medium-low maturity, and form effective pore-fracture networks for hydrocarbon transport together with multi-type and multi-scale microfractures. Self-sealing capacity of shale is conducive to the in-situ or proximal preservation of shale oil and gas. Comparison of typical continental shale sequences in the Chinese sedimentary basins indicates that favorable source-reservoir coupling, suitable thermal maturity level, and self-sealing capacity of shale are the major controls for oil enrichment in lacustrine shale. This study also presents a preliminary model for differential enrichment of lacustrine shale oil in China. Therefore, the laminated shales in medium-low maturity in gentle slope zones and the clayey shale-rich strata in medium-high maturity in deep sags should be prioritized in lacustrine shale oil exploration in downfaulted lacustrine basins. Moreover, both the shale interbedded/intercalated with sand and the clayey shale in medium-high maturity are crucial to making breakthroughs in lacustrine shale oil exploration therein.

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    Concept, method and prospect of molecular oil recovery
    Bingyu JI, Jichao FANG, Shu YANG, Yong HU
    Oil & Gas Geology    2023, 44 (1): 195-202.   DOI: 10.11743/ogg20230116
    Abstract298)   HTML11)    PDF(pc) (3961KB)(138)       Save

    The understanding and control at molecular level has become an inevitable trend in the development of modern science and technology, but it has not attracted enough attention in the field of oil and gas development. Based on some achievements and understandings of molecular simulation, this paper puts forward the concept of molecular oil recovery (molecular gas recovery) for the first time, and analyzes its connotation, current situation and development trend. Relevant research achievements in surfactant flooding, polymer flooding and CO2-EOR have been documented and enriched the connotation of molecular oil recovery to a certain extent. Relying on molecular simulation technology represented by molecular dynamics and quantum chemical calculation combined with modern experimental technology represented by chromatography, spectroscopy, mass spectrometry, and nuclear magnetic resonance, etc., it is possible to deepen the understanding of the mechanism of viscosity formation and viscosity reduction of heavy oil, and the characteristics of oil and gas adsorption, desorption and slippage on rock surface from the molecular level. In this way, a new mechanism based on molecular oil recovery is proposed, and the molecular structures of more targeted viscosity reducer, oil displacement agent, plugging agent and other auxiliary materials are designed. Molecular oil recovery technology based on molecular simulation methods is expected to bring revolutionary advances to the research of chemical oil displacement mechanism, thermal recovery mechanism, CO2 displacement mechanism, low salinity water displacement mechanism, shale oil and gas exploitation mechanism and natural gas hydrate exploitation mechanism, etc., providing theoretical support for efficient oil and gas recovery methods.

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    Characteristics and influencing factors of adhesive force between hydrate particles and mineral surface
    Ying Teng, Pengfei Wang, Zachary Aman
    Oil & Gas Geology    2022, 43 (3): 703-710.   DOI: 10.11743/ogg20220318
    Abstract298)   HTML10)    PDF(pc) (2082KB)(204)       Save

    In the process of hydrate mining, the droplets and bubbles in pipeline can be turned into hydrate particles under the environmental conditions. The occurrence of hydrate particle aggregation can cause blockage, leading to potential safety problems. Adhesive force is the key to exploring the flow safety of mining pipeline and the accumulation/deposition mechanism of hydrate particles. At present, the relevant researches focus on the measurement and characterization of the adhesive force between hydrate particles or between particles and surface in transport process. However, documents on the effects of mineral wettability and surface roughness on the adhesion of hydrate deposits are rarely seen. In this study, the adhesive force between hydrate particle and carbon steel surface treated by different methods as well as mineral surface, such as quartz, malachite, calcite and kaolinite were measured and analyzed using the adhesive force measurement experimental system. The results show that the adhesive force of hydrate particles to mineral surface is 3-6 times that of hydrate particles to carbon steel surface, due to the wettability difference. In addition, the adhesive force between hydrate particles and mineral surfaces is also affected by contact time, as shown by the strengthened adhesive force of hydrate particles with calcite and kaolinite surfaces under prolonged contact. The effects of ionic surfactants on hydrate growth rate and adhesion were also investigated, and it was pointed out that the change of contact area between particles and water film on mineral surface serves to change the morphology of hydrate particles from layered structure to needle-like structure. Finally, in comparison of the experimental results with theoretical calculation, we concluded that the strong hydrophilicity of the mineral surface is key to the differences.

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    Progress and research direction of EOR technology in eastern mature oilfields of Sinopec
    Li Zhang
    Oil & Gas Geology    2022, 43 (3): 717-723.   DOI: 10.11743/ogg20220320
    Abstract297)   HTML15)    PDF(pc) (513KB)(306)       Save

    In view of the characteristics and challenges in developing the eastern mature oilfields of Sinopec, the study focuses on major progress made in research of enhancing oil recovery (EOR) technologies such as water flooding, chemical flooding, thermal recovery of heavy oil and CO2 flooding, and introduces the application effects. For water flooding, focus is put on improvement of local injection-recovery relation, being combined with separate intelligent separate-layer injection and production technology, and pressurized water injection experiment is carried out in ultra-low permeability reservoirs. For chemical flooding, the binary surfactant/polymer flooding and the heterogeneous phase combination flooding (HPCF) have been developed and applied, with calcium/magnesium-tolerant agents developed for oil reservoirs with high temperature and high salinity. In terms of heavy oil reservoirs, compound viscosity-reducing flooding has been implemented in reservoirs with low displacement efficiency, H(horizontal well)+D(viscosity reducer)+C(CO2)+S(steam) technology in deep ultra-heavy oil reservoirs, H (horizontal well)+D(viscosity reducer)+N(N2)+S(steam) technology in shallow ultra-heavy oil reservoirs, chemical steam flooding in deep heavy oil reservoirs. As for CO2 flooding, long-effect soaking and large slug injection technology has been put into effect in high-permeability reservoirs with high water cut; high-pressure and low-rate injection and alternate injection of water and gas from different wells in low permeability/ultra-low permeability reservoirs; and asynchronous cyclic injection and production in tight reservoirs. Analysis of the progress mentioned above serves for indicating the development direction of EOR promotion in different types of reservoirs.

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    Oil enrichment law of the Jurassic Yan’an Formation, Hongde block, Longdong area, Ordos Basin
    Shuai Yin, Zhonghu Wu, Xiaoming Wu, Jianping Liu, Chengqian Tan, Ruyue Wang, Hui Yuan, Yawei Dai
    Oil & Gas Geology    2022, 43 (5): 1167-1179.   DOI: 10.11743/ogg20220513
    Abstract294)   HTML12)    PDF(pc) (13857KB)(131)       Save

    The Jurassic in the Hongde block, Longdong area, Ordos Basin, has been less explored until some oil discoveries were made in the same system of nearby blocks. The Yan’an Formation in the Hongde block is taken as the subject of study to reveal conditions for possible oil accumulations in the formation based on relevant core, logging, seismic and testing data as well as analyses of sedimentary systems, tectonics and paleo geomorphology-the three most likely controlling factors for oil pooling. The results indicate that from the Yan’an Formation to the Yanchang Formation in the area there are three local unconformities respectively between the Fuxian Formation and the Yanchang Formation, the Yan 10 sub-member (Yan’an Formation) and Yanchang Formation, and the Yan 9 sub-member (Yan’an Formation)and Yanchang Formation. Five types of pre-Jurassic paleomorphologic units are also recognized:the paleovalley, inter-channel hill, ancient terrace, slope belt and low residual hill. Among them, the slope belt and low residual hill are conducive to hydrocarbon accumulation,and the ancient terrace and valley in the Yan 10 sub-member also have certain hydrocarbon accumulation potential. In addition, favorable conditions for oil accumulation also exist in the slope mouth where sandbodies have low shale content as several tributaries converged here and washed shale away. Oil caps and oil-water contacts are easily recognized. From a plan view, fault zones are intersecting sandbodies. The hanging walls of faults form perfect traps for oil, while the footwalls, without effective sealing, are usually barren in terms of oil pool. Normal faults are comparatively better oil pool holders than reverse ones. High-quality sedimentary reservoirs are necessary but insufficient conditions for the Yan’an Formation to contain oil pools. Based on the understanding, a method for identifying reservoirs in the Jurassic Yan’an Formation in the Hongde block is proposed.

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    Technologies and prospect of full-cycle development of low-permeability tight gas reservoirs with horizontal wells, Ordos Basin
    Jinbu LI, Yuehua CUI, Yougen HUANG, Shixiang FEI
    Oil & Gas Geology    2023, 44 (2): 480-494.   DOI: 10.11743/ogg20230218
    Abstract294)   HTML26)    PDF(pc) (5208KB)(200)       Save

    The geological characteristics of low-permeability tight gas reservoirs (developed mostly with horizontal wells) in the Ordos Basin are systematically described based on previous gas development experiences. A successful development of these reservoirs with horizontal wells usually comprises four stages based on a study of the targets, technical parameters, and performance indicators of the wells: exploring all possibilities, tackling technical problems, scaling up of technology implementation as well as optimization and improvement. The technical connotation of horizontal well development in Ordos Basin is elaborated and represented by a series of development technologies including multidisciplinary sweet spot optimization technology, overall deployment technology of multi-layer large well cluster, multidisciplinary integrated geosteering technology, and fine fracturing technology with a full life cycle production management. A comprehensive evaluation of gas development through horizontal wells from different types of gas reservoirs indicates that horizontal wells perform better in tight gas reservoirs, that strengthening the joint efforts on multi-disciplinary research for the whole process is the main direction of horizontal well technology development as well as the key to a large-scale development of low-grade natural gas resources with profit. For developing reservoirs with more complex conditions such as those buried deep in thin layers with low abundance of gas, horizontal wells will be further improved to deal with the challenges in the brown Sulige gas field where targeted optimization of the technology will be carried out, the green gas fields such as Qingyang and Yichuan where supporting technology will be developed, and the new forms of gas resources such as shale gas, coal-bed methane, etc, that require effective development technologies, thus ensuring a steady increasing gas production in the Ordos Basin.

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    Sequence stratigraphy models of carbonate-evaporite successions and their controls on source rocks and reservoirs in the Ordovician Majiagou Formation, Ordos Basin
    Tao ZHANG, Yaxiong ZHANG, Xiaohui JIN, Yan ZHOU, Juntao ZHANG, Ning GU, Wei ZHANG, Ruyue WANG, Kai LU
    Oil & Gas Geology    2023, 44 (1): 110-124.   DOI: 10.11743/ogg20230109
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    Based on the existing research results and the classical sequence stratigraphy theory of Vail P. R., this study takes into account the sedimentological principle of carbonate-evaporite, platform morphology, and lithological association characteristics of basin interior and margins to propose a sequence stratigraphic division model for the Majiagou Formation in Ordos Basin. According to the model, the sequence, which consists of evaporites mainly at the lower part and shallow water carbonates in the upper part, can be divided into five third-order sequences with boundaries respectively at the bottom of members of Ma1, Ma3, Ma510, Ma56, and Ma54. The bottom and top of Majiagou Formation are regional unconformity surfaces. Within the duration of lowstand systems tract of these third-order sequences, the carbonates and evaporite interfinger each other. The number of the evaporite layers is related to the number of hiatus (unconformity) in the adjacent carbonate sequences. The existence of these 4-5th order hiatus (unconformities) is the prerequisite for the development of interlayer dissolution and determines the location of source rock layers of inter-evaporite. Potential hydrocarbon source rocks are likely to be developed in three evaporative sequences of Ma1, Ma3 and Ma56 members in the lowstand systems tract, which are mainly distributed in the lows surrounding the salt lake and the slope areas of the basin center; moreover, are characterized by thin layers and large accumulated thickness. The sedimentary facies and multi-order sequence boundaries control the development of reservoirs, and two types of reservoirs are mainly formed: (1) The porous dolomitic reservoirs of beach facies are mainly developed in the middle and upper parts of highstand systems tract (HST) of third-to-fourth-order sequence, and the superimposed areas of the sedimentary hiatus and beach facies are the favorable zones for the porous reservoirs. (2) The moldic pore-type gypsodolomite reservoirs are mainly developed during the secondary transgression of the lowstand systems tract, and the tidal flat facies zone in the basin margins surrounding the paleo-uplift are the favorable horizons for the development of reservoirs of moldic pore type.

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    Lithofacies types and reservoir characteristics of Jurassic shale in the Sichuan Basin revealed by the Da’anzhai Member, Well Y2, Yuanba area
    Qianwen Li, Zhongbao Liu, Feiran Chen, Guangxiang Liu, Dianwei Zhang, Peng Li, Pengwei Wang
    Oil & Gas Geology    2022, 43 (5): 1127-1140.   DOI: 10.11743/ogg20220510
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    The continental shale strata are generally lithologically complicated and highly heterogeneous, making it difficult to pinpoint sweet spots and deploy exploratory wells. To evaluate the reservoir characteristics and gas-bearing capacity of different lithofacies types of Jurassic shale sequences in the Sichuan Basin, the Da’anzhai Member (Well Y2) in the Yuanba area was taken as an example. Experimental methods including TOC content measurement, whole-rock mineral composition analysis, thin section observation, FIB-SEM, mercury injection-N2 adsorption measurements as well as tests for physical properties were performed to classify the lithofacies types of shale and interlayers in the second sub-member of the Da'anzhai Formation (hereinafter referred to as the J1da2) and then to single out the lithofacies or lithofacies assemblages with the highest hydrocarbon potential based on physical properties, pore structure, gas content and occurrence as well as fracability. Results show that the shale can be divided into three categories and six sub-categories of lithofacies types, and the interlayers into two categories and six sub-categories for lithofacies types, which can be further grouped into three lithofacies assemblage types from a macro perspective. The shale contains mostly inorganic pores such as interlayer pores within clay minerals and dissolved pores of calcite, providing storage space for gas. The total shale gas content is calculated to be 2.59-4.38 m3/t, in which the free gas accounts for an average of 67 %, indicating a good exploration potential. However, the brittle mineral content of shale lithofacies is barely 50 %, indicating a poor fracability. It is concluded that type AB-Ⅰ lithographic assemblages in the sub-member are the most promising exploration targets as they are observed to contain well developed cleavage and lamellation fractures, favorable hydrocarbon generation conditions, higher gas content and proportion of free gas as well as brittle interlayers, all indicating the most promising exploration targets of all types.

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    Characteristics of hydrocarbon source-migration-accumulation in Huizhou 26 Sag and implications of the major Huizhou 26-6 discovery in Pearl River Mouth Basin
    Hesheng Shi, Yangdong Gao, Jun Liu, Junzhang Zhu, Zulie Long, Yuling Shi
    Oil & Gas Geology    2022, 43 (4): 777-791.   DOI: 10.11743/ogg20220404
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    In the Pearl River Mouth Basin, a majority of hydrocarbons were discovered in the Miocene-Oligocene reservoir rocks deposited during the depression stage, while only 8 % of the discovered hydrocarbons were found in the Eocene reservoir rocks formed during the rifting stage, and no commercial discoveries have been made in the Mesozoic buried hills. The main problems in exploration for the Paleogene reservoir rocks and Mesozoic buried hills include whether there are a quantity of hydrocarbons still preserved in the middle-to-deep downfaulted reservoir rocks of hydrocarbon-rich sags, whether the hydrocarbon migration pathways are effectively developed in the Paleogene reservoir rocks and Mesozoic buried hills, as well as whether the hydrocarbon accumulation dynamics, traps and reservoir-seal assemblages are well developed. In line with the assessment theory of “source-migration-accumulation”, the study discusses the static and dynamic elements of the hydrocarbon accumulation system in Huizhou 26 Sag, Pearl River Mouth Basin, including the hydrocarbon source in terms of types and quality of source rocks, thermal evolution and hydrocarbon generation-expulsion history, and types and scale of hydrocarbon resources, the hydrocarbon migration in terms of migration unit and direction, migration pathway, confluence intensity, as well as the hydrocarbon accumulation in terms of secondary structural belt and trap, reservoir-seal assemblage, charging intensity and preservation condition. In conclusion, the study reveals the characteristics of source-migration-accumulation for the Paleogene reservoir rocks and Mesozoic buried hills in Huizhou 26 Sag, sets up a dynamic accumulation model featuring “accelerated maturation of oil-prone source rocks at later stages, generation of oil at first followed by gas, joint control of fault and overpressure, strong hydrocarbon supply by source-reservoir juxtaposition, and 3D migration and accumulation”. Major breakthrough has been made thereby in the exploration for the Paleogene reservoirs and Mesozoic buried hills in Huizhou 26-6 structure.

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    Physical property and heterogeneity of tight sandstone reservoirs: A case of the Upper Triassic 6th member of Xujiahe Formation, Guang’an, central Sichuan Basin
    Liang Yue, Qingqiang Meng, Ziliang Liu, Wei Yang, Hui Jin, Fang Shen, Junjian Zhang, Sibing Liu
    Oil & Gas Geology    2022, 43 (3): 597-609.   DOI: 10.11743/ogg20220309
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    Unconventional tight sandstone reservoirs with proven natural gas reserves up to trillion cubic meters are typical of the Upper Triassic Xujiahe Formation of clastic rocks in the Sichuan Basin of southwestern China. The 6th member of Xujiahe Formation (Xu 6 Member) in Guang’an area, central Sichuan Basin, contains gas reservoirs with great exploration and development potential. In this study, thin section observation, physical property measurements, mercury intrusion tests and fractal theory were integrated to analyze a suite of the Xu 6 Member tight gas sandstone samples in terms of pore structure, physical property and reservoir heterogeneity. The results show that the sandstone reservoirs studied can be classified into three types. That is, TypeⅠreservoir (with an average porosity of 12.27 % and average permeability ratio of 6.037 6 × 10-3 μm2) is dominated by macro- or meso-scale pores, and its fractal dimension varies between 2.42 and 2.59. TypeⅡreservoir (with an average porosity of 9.26 % and average permeability ratio of 1.152 3 × 10-3 μm2) is dominated by meso-scale pores, followed by micro-scale pores, with macro-scale pores poorly developed; and its fractal dimension ranges from 2.47 to 2.56. TypeⅢreservoir (with an average porosity of 5.20 % and average permeability ratio of 0.351 7 × 10-3 μm2) is dominated by micro- or meso-scale pores, together with poorly developed or undeveloped macro-scale pores; and its fractal dimension varies between 2.45 and 2.81. The different distribution of pore types leads to obvious changes in the heterogeneity of various types of reservoirs, which mainly shows that the heterogeneity of TypeⅢreservoir is stronger than that of TypeⅠreservoir. Differential distribution of pore types is directly related to reservoir heterogeneity, as manifested by stronger heterogeneity of TypeⅢreservoir compared with TypeⅡ. Correlation analysis reveals that differential pore types are coupled with reservoir heterogeneity, and there is a critical value. When the fractal dimension ranges between 2.45 and 2.60, the porosity and fractal dimension are in positive correlation, and the variation of permeability is irregular; when the parameter is greater than 2.60, there is a negative correlation between porosity and fractal dimension, and permeability is in linear relationship with fractal dimension with a slope close to 0. In all, the quantitative study on physical properties and fractal characteristics of tight sandstone reservoirs, is of great theoretical and practical significance to discussing the evaluation criteria of unconventional high-quality natural gas reservoirs, and guiding the exploration and development of unconventional reservoirs in China.

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    Characterization of sequence architectures and sandbody distribution in continental rift basins
    Xiaomin Zhu, Hehe Chen, Jiawang Ge, Mingxuan Tan, Qianghu Liu, Zili Zhang, Yaxiong Zhang
    Oil & Gas Geology    2022, 43 (4): 746-762.   DOI: 10.11743/ogg20220402
    Abstract290)   HTML36)    PDF(pc) (8988KB)(232)       Save

    Efficient oil and gas exploration and development in petroliferous continental rift basins relies heavily on a profound understanding of sequence stratigraphic architectures and sandbody distribution characteristics in different tectonic evolution stages. Based on a review of the development status of sequence stratigraphy and geological characteristics of continental rift basins, this study characterizes the sequence stratigraphic architectures and sandbody distribution according to a four-stage tectonic evolution of the basins: ① During the early syn-rift stage, faulting at basin boundaries starts with parasequences being vertically aggraded and superposed, and with near-source coarse-grained depositional systems including alluvial fan, distributary channel, and fan delta being developed. ② During the main syn-rift stage, faulting intensifies with parasequences showing a variety of overlapping styles in different structural belts and systems tracts, and basins fill mainly with fluvial, delta and gravity flow. ③ During the transition stage from rifting to depression, faulting starts to wean with parasequences being overlapped and dominated by progradation and aggradation, and depositional systems dominated by axial fluvial and deltaic depositional systems being developed. ④ During the post-rift depression and subsidence stage, faulting nearly ends with basins in an overcompens and with the fluvial-shallow-water deltas being developed. Current hot topics and future development of sequence stratigraphy in continental rift basins are also discussed based on the above analyses.

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    Study and practice of characterizing hydrocarbon charging capacity of different fault zones, Shunbei area, Tarim Basin
    Wenge Hu
    Oil & Gas Geology    2022, 43 (3): 528-541.   DOI: 10.11743/ogg20220304
    Abstract289)   HTML18)    PDF(pc) (9529KB)(184)       Save

    The Middle-Lower Ordovician carbonate reservoirs along strike-slip fault zones in the Shunbei area, Tarim Basin, are hydrocarbon bearing and have been the main targets of exploration and development for oil and gas. However, hydrocarbon charging efficiency at difference parts of the zones varies greatly, posing challenge for accurately evaluating and describing the dominant parts of charging, which in turn determines the efficiency and scale of exploration and development in the Shunbei area. To tackle the problem, this study is focused on the relationship between the faults and reservoirs in two of the fault zones (No.1 and 5) to discuss for the first time the main factors affecting the hydrocarbon charging efficiency in the zones that are reflected through the internal structure of the zones, the local strain intensity as well as the size and direction of the present in-situ stress. Based on the study, the concept of “charging body” is proposed and implemented to semi-quantitatively determine the vertical transport of hydrocarbons at different parts of the zones with results fitting well with the actual production data. This method not only provides strong theoretical support for segmental assessment of the zones and description of “high-speed channels” for vertical hydrocarbon migration, but also serves as a guidance to rapidly increasing reserves and promoting production with less wells in the Shunbei area.

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    Complex gas-water contacts in tight sandstone gas reservoirs: Distribution pattern and dominant factors controlling their formation and distribution
    Jianhui ZENG, Yaxiong ZHANG, Zaizhen ZHANG, Juncheng QIAO, Maoyun WANG, Dongxia CHEN, Jingli YAO, Jingchen DING, Liang XIONG, Yazhou LIU, Weibo ZHAO, Kebo REN
    Oil & Gas Geology    2023, 44 (5): 1067-1083.   DOI: 10.11743/ogg20230501
    Abstract289)   HTML49)    PDF(pc) (4999KB)(366)       Save

    In recent years, extensive exploration and exploitation activities in tight sandstone gas reservoirs have highlighted the common phenomenon of water production, indicating complex gas-water contacts. Exploring gas layers while avoiding water layers has become critical to the efficient exploration and exploitation of tight sandstone gas reservoirs. This study presents comprehensive geological analyses of gas-water contacts in simple gentle tectonic zones (tight sandstone gas reservoirs in the Sulige and Daniudi areas in the Ordos Basin), a transition zone of simple gentle to complex uplift (Hangjin Banner in the Ordos Basin), and complex uplift zones (tight-gas reservoirs in the western Sichuan Basin). Combined with the core-scale and pore-scale physical simulations of gas-water contact in tight sandstone, we clarify the types and characteristics of gas-water contacts in tight-gas sandstone reservoirs, reveal the dominant factors controlling the formation and distribution of intricate gas-water contacts based on the sand bodies, cores, and pores, and establish corresponding gas-water distribution patterns. Key findings are as follows. In terms of sand body, there are primarily six types of gas-water contacts within, including (1) the simple type of gas layer without water layer; (2) the normal type with gas layer underlain by water layer; (3) the inverted type with gas layer overlaid by water layer; (4) the hybrid type with gas and water in the same layer; (5) the isolated type with water layer within a gas layer; and (6) the simple type of water layer without gas. The distribution range, style, and boundary of gas-water contacts are governed by hydrocarbon-generating intensity, reservoir heterogeneity, and a combination of source rock-reservoir pressure differences and tectonic activity, respectively. At core-scale, permeability coupled with charging dynamics of the tight sandstone governs the critical conditions for the formation and distribution of gas-water contacts. At pore-scale, the coupling of pore throat size and coordination number with charging pressure dictates the fluid occurrence and seepage characteristics, determining the critical conditions for the formation and distribution of gas-water contacts. Owing to the collective effects of dominant factors from sand body, core-scale, and pore scale and their differences, tight-gas reservoirs with different source rock-reservoir assemblages exhibit different gas-water distribution patterns.

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    Mechanical characteristics and fracture propagation mechanisms of the Gulong shale
    He LIU, Siwei MENG, Suling WANG, Kangxing DONG, Liu YANG, Jiaping TAO, Lihao LIANG
    Oil & Gas Geology    2023, 44 (4): 820-828.   DOI: 10.11743/ogg20230402
    Abstract288)   HTML34)    PDF(pc) (9060KB)(348)       Save

    The Gulong shale oil represents China’s first attempt at large-scale exploration and exploitation of the oil contained in shale sequences without intercalations. Clarifying the rock mechanical characteristics and fracture propagation mechanisms of the Gulong shale is vital for guiding the selection of landing zones and fracturing design and engineering parameter optimization. In this study, the mineral distribution, thin section observation and rock mechanics tests are performed to clarify the Gulong shale as “fine layered” texture in mechanics and reveal the fracture propagation mechanisms under the control of multiple geological and engineering factors. It is shown that the Gulong shale is characterized by high clay mineral content (Avg. 46.6 %), strong plasticity, a foliation intensity of up to 1 000~3 000 stripes per meter and strong mechanical anisotropy. Unlike the brittle fracturing of conventional shale, the typical rock samples from Gulong exhibit high-frequency fluctuation in mechanical property, with a fluctuation frequency of 3.33 times per cm for a compressive strength greater than 20 MPa. The fracturing process is observed as a steady gradual process with a slow post-peak stress decline, and along a random path in a zigzagged shape. Meanwhile, in the case of high-density foliation fractures, the hydraulic fractures in the Gulong shale are of complex morphology, with their height and length being significantly constrained. The limited vertical and horizontal extension of hydraulic fractures has been a major constraint for the effective stimulation of the Gulong shale oil reservoir. It is thereby suggested that the hydraulic stimulation of the Gulong shale oil reservoir should follow the principle of controlling near-wellbore fracture branching and further extending distal fracture networks, while placing the fracturing treatment under more effective control to suppress the development of near-wellbore fractures and boost the extension of main fractures to sufficiently expand the stimulated reservoir volume.

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