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Table of Content

    08 June 2014, Volume 35 Issue 3
    Gas accumulation and exploration direction of the Permian and Triassic reservois of reef-bank facies in Sichuan Basin
    Guo Xusheng, Huang Renchun, Fu Xiaoyue, Duan Jinbao
    2014, 35(3):  295-302.  doi:10.11743/ogg20140301
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    Through systematic analysis of gas component,carbon isotope,thin section and inclusions,we found that the Permian and Triassic reef-bank reservoirs are dominated by natural gas from secondary cracking of crude oil.The Longtan Formation(Wujiaping Formation)is the major source rocks.The gas reservoirs experienced three stages,namely earlier oil accumulation in ancient lithologic reservoirs,ancient crude oil cracking and gas adjusting and re-accumulation.The hydrocarbon accumulation pattern is characterized by multiple hydrocarbon supply,accumulation near the source,lithology reservoirs,oil-gas conversion and later adjustment.And the present day gas reservoirs are mainly controlled by three factors.Firstly,the hydrocarbon kitchen of the Permian source rock controls the adequacy of oil-gas source.Secondly,the distribution and scale of reservoirs of reef-bank facies control the scale and location of hydrocarbon accumulation.Thirdly,later preservation conditions determine the finally accumulation of gas.By systematically summarizing the sedimentary characteristics and hydrocarbon accumulation conditions of the discovered reef-bank gas reservoirs(outcrops),we believe that reservoirs of platform margin reef-bank facies,intra-platform shoal facies and the Lower Permian shoal facies are the favorable targets for further gas exploration.

    Tectonic evolution,sedimentary system and petroleum distribution patterns in dustpan-shaped rift basin:a case study from Jiyang Depression,Bohai Bay Basin
    Song Guoqi, Hao Xuefeng, Liu Keqi
    2014, 35(3):  303-310.  doi:10.11743/ogg20140302
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    The sedimentary basins in eastern China(like Jiyang Depression)are characterized by dustpan-shape with marginal faults and vertical overlapping architecture.These basins formed due to the subduction of Pacific Plate under China continent,which caused crust stretching and thinning,and further resulting in a series of extension of faults.In dustpan-shaped rift basin,the tectonic intensity varies in different structural belts.Therefore,the sedimentary systems and their assemblages under their control correspond well with the palaeogeomorphology.Due to the control of tectonic evolution and depositional characteristics,the traps,carrier system and the accumulation dynamics show some orderliness of distribution,which determines the orderliness of reservoir type distribution.Secondly,the differences of the major hydrocarbon accumulation controlling factors and their assemblages between different structure belts generate the differences of hydrocarbon accumulation and reservoir patterns between different plays.Moreover,different types of subtle reservoirs are deve-loped at different structural belts.Specifically,conglomerate fan reservoirs in the steep slope belt show hydrocarbon accumulation pattern featured by diagenetic sealing.The turbidity fan reservoirs in the central-depression belt show the hydrocarbon accumulation pattern featured by pressure-subtle migration.And the beach-bar sand bodies in the gentle slope belt show hydrocarbon accumulation pattern featured by control of three elements,i.e.faulted structures,effective reservoir,and formation fluid pressure.In conclusion,the petroleum geologic features of the Paleogene dustpan-shaped rift basins in east China can be sum up as follows:regularity in the evolution of basin,correspondence in sedimentary system,orderliness of reservoir type distribution,and difference in key factors controlling hydrocarbon accumulation.

    Forming conditions and hydrocarbon accumulation patterns of the Neogene low resistivity reservoirs in low-amplitude structure of Qionghai Salient
    Gan Jun, Zhang Yingzhao, Deng Guangjun, Lu Jiang, Zheng Rongfen
    2014, 35(3):  311-316,349.  doi:10.11743/ogg20140303
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    Using geochemical,sedimentary and hydrocarbon accumulation analysis methods,this paper studied the characteristics of source rocks,hydrocarbon migration and accumulation of the low resistivity reservoirs of the 1st Member of Zhujiang Formation(Zhu1)in the low-amplitude structure of Qionghai salient in Wenchang-13 block,Qionghai salient.The following results were obtained.The oil of the Zhu1 low resistivity reservoir in Wenchang 13-X is mainly sourced from the shallow lacustrine mudstone of Enping Formation in Wenchang sag,which is another high quality source rock in addition to the Wenchang Formation mudstone of mid-deep lacustrine faciesin.The low resistivity reservoirs of Zhu1 in Wenchang13 block are of structural-lithologic composite type developed in the low amplitude drape anticlines.The main reservoir consists of offshore fine muddy siltstone with fine grain and high mud content,which are the main causes of the low resistivity.The low resistivity reservoirs area characterized by low amplitude structure and low permeability.The low resistivity reservoirs are secondary accumulation with hydrocarbons sourced from the underlying high resistivity reservoir.The low resistivity and high resistivity reservoirs superimpose vertically to form a hydrocarbon enrichment zone.The low resistivity reservoirs in low amplitude structure are important targets for potential-tapping in mature area.

    Genesis and composition of ‘baseline hump’ in biodegraded oil samples from Biyang Depression
    Guo Pengfei, He Sheng, Zhu Shukui, Chai Derong, Zhang Wanfeng, Dai Wei, Zhang Junli
    2014, 35(3):  317-325.  doi:10.11743/ogg20140304
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    Five biodegraded oil samples from the north slope of Biyang Depression were analyzed by integrating the two-dimensional gas chromatography/time-of-flight mass spectrometry(GC×GC/TOFMS),gas chromatography(GC)and gas chromatography-mass spectrometry(GC-MS)to reveal the composition and genesis of ‘baseline hump’.All the oil samples analyzed are of similar original compositions and thermal maturities,but different degradation levels at 2,3,5,6 and 8,respectively.With the increasing of oil degradation level,n-alkanes,iso-alkanes,aromatic hydrocarbons with low molecular weight,steranes,terpanes and polycyclic aromatic hydrocarbons are degraded successively,resulting in the significant decrease of the number of compound types.The cyclic alkanes and isomers with similar polarities and strong resistance to biodegradation are enriched relatively in the biodegraded oil,and their co-elution in GC chromatograms results in ‘baseline hump’ or so-called ‘unresolved complex mixtures (UCMs)’.Total 2D characteristic mass spectrums and standard compound tests show that cyclic alkanes and their homologues are the major components of the UCMs,with a basic framework of cyclohexane.Additionally,the UCMs can be divided into six types(typeⅠto typeⅥ).The typeⅠandⅡare composed of C16-C26 long chain alkyl-cyclohexanes,C11-C16 alkyl-decalins and their isomers.These cyclic alkanes with one or two rings might be the new compounds from the microbial transformation of normal oils.Type Ⅲ-Ⅵ are composed of sesquiterpenoids,tricyclic terpanes,low molecular weight steranes,diasteranes and norhopanes,originated from the enrichment of hydrocarbons having relatively strong resistantance to degradation in the normal oils.

    Characteristics and depositional models of source rocks in Langgu Sag,Bohai Bay Basin
    Diao Fan, Zou Huayao, Hao Fang, Jin Fengming, Sun Yehua, Luo Qing, Shi Yulei, Liang Xiaojuan
    2014, 35(3):  326-335.  doi:10.11743/ogg20140305
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    Rock-Eval data,carbon and oxygen isotopes and molecular geochemical parameters of the source rocks in Es4(the 4th member of Paleogene Shahejie Fm)-the lower Es3(the 3rd member of Paleogene Shahejie Fm)in Langgu Sag were integrated to study the formation mechanism of lacustrine source rocks with low abundance under different tectonic and climatic conditions.Rock pyrolysis and kerogens' maceral composition analysis revealed that the Es4 and the lower Es3 are the similar in the major kerogen type of Ⅱ,but are quite different in organic matter abundance.Based on analyses of carbon and oxygen isotopes in the context of regional tectonic and palaeo-climate settings,we established depositional models for the source rocks in Es4-lower Es3.The source rock in the Es4 was deposited in a lake basin at the initial stage of rifting,with low width/depth ratio,arid climate,and brackish water or saline water with stable salinity stratification.Its 13C-depleted of the inorganic and organic matter and lower Pr/Ph might reflect relatively low primary productivity and better organic preservation.In contrast,the source rock in the lower Es3 was deposited in a lake basin in the intense rifting stage,with a high width/depth ratio,warm and humid climate,fresh water,and frequent water-column overturning with unstable temperature stratification.Its 13C enrichment of the inorganic and organic matter and C27/C29 sterane ratios were interpreted to be caused by higher primary productivity and more terrigenous organic matter input.

    Comparison of hydrocarbon generation conditions between lacustrine and marine carbonate source rocks
    Tian Chuntao, Ma Suping, Yang Yan, Meng Jun, Xia Yanqing
    2014, 35(3):  336-341.  doi:10.11743/ogg20140306
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    The differences of hydrocarbon-generating conditions of lacustrine and marine carbonate source rocks were discussed in various aspects,such as the distribution characteristics,sedimentary environment,rock type,organic geochemical characteristics and hydrocarbon generation mode.The results show that marine and lacustrine carbonate source rocks all containe varying amounts of argillaceous components and are dominated by kerogen of typeⅠor type Ⅱ.In addition,there is no significant difference in occurrence of their organic matter,except for that lacustrine carbonate source rocks contain more amorphous organic matters.Organic carbon content of marine carbonate rocks is generally low,while that of lacustrine carbonate rocks is highly variable.The research of the hydrocarbon generation mode of lacustrine carbonate source rocks is still very weak in comparison with the marine carbonate source rocks,and the secondary hydrocarbon generation of the former should not be neglected.The formation conditions of lacustrine carbonate source rocks are controlled by many factors,the biogeochemical and sedimentological researches of lacustrine carbonate source rocks with high content of organic matters are especially important.Furthermore,the possibility of late hydrocarbon generation of lacustrine source rocks providing sufficient hydrocarbon sources for deep reservoirs of lacustrine faices is one of the important topics for future study.

    Total sulfur distribution of source rock of the Upper Permian Longtan Formation and its response to sedimentary environment in Sichuan Basin
    Fu Xiaodong, Qiu Nansheng, Qin Jianzhong, Tenger, Liu Wenhui, Wang Xiaofang
    2014, 35(3):  342-349.  doi:10.11743/ogg20140307
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    Based on the systematic analysis of Total Sulfur content(TS)of source rock from the Upper Permian Longtan Formation(LTF)in Sichuan Basin,this paper studied the distribution feature of TS,its controlling factors as well as its responses to and significance as a indicator for sedimentary environment.Shale source rock of LTF is rich in sulfur,but limestone is poor in sulfur.TS has positive correlations with TOC,pyrites content and δ13C value of kerogen respectively.The TS and TOC/TS value of source rock have distinct responses to and significance as indicators for the sedimentary environment. Source rocks of LTF in paralic facies in middle and southern Sichuan Basin has high TS and low TOC/TS value.Source rocks in intra-platform sag or deep-water shelf facies in northeastern Sichuan Basin has relatively higher TS and TOC/TS value.And limestone in carbonate platform or shallow-water carbonate shelf facies in Chengkou,Nanjiang,Shizhu areas located at the edge of Sichuan Basin has low TS and high TOC/TS value.

    Application of fluid inclusion techniques to the study of super-heavy oil accumulation in Chunfeng oilfield,Junggar Basin
    Xi Weijun, Zhang Zhihuan, Xu Xinyu, Shi Cui'e
    2014, 35(3):  350-358.  doi:10.11743/ogg20140308
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    The Chunfeng oilfield is located in the Chepaizi uplift of the northwestern margin of Junggar Basin.The heavy oil reservoir is characterized by shallow burial,multiple oil-bearing layers,high oil density and viscosity.The biomarkers generally experienced strong degradation,making it hard to perform oil-source correlation and study of oil accumulation.In this paper,we used experimental methods to analyze fluid inclusion's composition,optical characteristics,occurrence features,homogenization temperature and salinity,performed oil-source correlation,and studied the accumulation period and process.The results show that the heavy oil was mainly sourced from the Permian source rocks in the Changji Depression,and the oil has experienced a slight biodegradation before accumulation and strong degradation later.Late charging also occurs in some wellblocks.At the end of Triassic,the Mid-Lower Permian source rocks had entered into peak oil generation and the oil generated from the Permian migrated to and accumulated in the Cheguai faulted belt.The tectonic movement during the end of Cretaceous to Paleogene destroyed and reconstructed the reservoir in the Cheguai faulted belt,and the hydrocarbons migrated to the Chepaizi uplift and accumulated in the Jurassic and Cretaceous reservoirs.Because of the poor preservation conditions,the oil commonly experienced strong biodegradation and was turned into heavy oil.Since the Neogene,the tectonic movement further adjusted the reservoirs in the Cheguai faulted belt,oil and gas migrated to Chepaizi uplift and accumulated in the favorable traps in Chunfeng oilfield and was biodegraded later into heavy oil reservoir.

    Research method of fault vertical sealing capacity in overpressure mudstone caprock and its application
    Hu Huiting, Wang Long, Liu Yan, Qin Peirui, Fu Hongjun
    2014, 35(3):  359-364.  doi:10.11743/ogg20140309
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    In order to study the role of fault in hydrocarbon accumulation and preservation,a comparative study was carried out on vertical sealing capacity of faults between overpressure and normal pressure mudstone caprocks.On this basis,displacement pressure of fault rock was calculated by using the empirical relationship between displacement pressure and shale content and buried depth.A set of methods for evaluating the vertical sealing capacity of fault in overpressure mudstone caprock was established and applied to Surennuoer fault zone of Wuerxun Sag in Hailar Basin.The displacement pressure of faults was quantitatively calculated,and the vertical sealing ability of overpressure mudstone caprock was eva-luated.The results indicate that K1d1 overpressure mudstone caprock has a weak sealing capacity in Surennuoer fault zone and is unfavorable for hydrocarbon accumulation and preservation.This result is in good agreement with the phenomenon that oil/gas are widely distributed in this fault zone but the reserves abundance is low.This shows that this method is feasible for quantitative calculation of the vertical sealing capacity of fault in overpressure mudstone caprock.

    Geochemical characteristics of paleofluid and hydrocarbon preservation in marine strata of Micang-Daba piedmont and its adjacent areas
    Li Fei, Shang Changjian, Lou Zhanghua, Zhu Zhenhong, Li Mei, Zhou Xiaoxing
    2014, 35(3):  365-371.  doi:10.11743/ogg20140310
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    Exploration for oil and gas in the marine strata of the Micang-Daba piedmont and its adjacent area turned out to be not so encouraging due to poor preservation conditions caused by multiple tectonic deformations.By characterizing carbon and oxygen isotopes and fluid inclusions in calcite veins in tectoclases,we tried to evaluate conditions for hydrocarbon preservation in these strata based on analyses of paleo-fluid,including origin,phases of activity and mixing of meteoric water.Results show that meteoric water infiltration increased progressively from the center to the edge of the basin and the infiltrating depth of the water was mostly between 1 200 and 3 000 meters in the piedmont.The homogenization temperature and salinity measurements of fluid inclusions indicate two phases of paleofluid activity corresponding respectively to the Yanshanian and Himalayan tectonic movements.During the Yanshanian movement,the meteoric water infiltration was weak and the marine strata in the study area had favorable preservation conditions for hydrocarbons.While during the Himalayan movement,the meteoric water infiltration was intensive.Together with a strong tectonic uplift and erosion,the infiltration made preservation conditions for hydrocarbon worse.

    Charateristics and exploration potential of Ordovician reservoirs in Sichuan Basin
    Guo Tonglou
    2014, 35(3):  372-378.  doi:10.11743/ogg20140311
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    The Ordovician has been the only strata with no comericial gas discoveries from the Sinian to Jurassic in Sichuan Basin.The Honghuayuan Fm.and the Tongzi Fm.of the Lower Ordovician share a similar sedimentary environment with the Longwangmiao Fm of the Cambrian and the Jialingjiang Fm of the Triassic,and the latter two formations were proven to contain large gas fields in their carbonates of grain beach facie.Based on an integrated analysis of drilling,seismic and regional geological data of the basin,we obtained the following conclusions.1)The lower Ordovician had the geological conditions needed for forming grain beach.The mound reflections on seismic profiles of southeastern Sichuan Basin are the responses of grain carbonate interbedded with gypsum and mudstone in the Tongzi Fm and the Honghuayuan Fm.2)There are two types of source rock-reservoir combinations in the Lower Ordovician,namely lower source rock-upper reservoir combination and upper source rock-lower reservoir combination.3)According to the exploration expe-riences in the Cambrian and Triassic of central Sichuan Basin,study should be performed in respects of sedimentary facies,paleo-geomorphology and hydrocarbon accumulation and evolution history with carrier system as the focus for exploration in the Ordovician.An exploration well should be emplaced in area with prominent anomaly reflections.

    Depositional evolution and genesis of K set of shelf sand ridges in the Zhujiang Formation of Huizhou sag,Pear River Mouth Basin
    Ding Lin, Zhang Changmin, Du Jiayuan, Shi Hesheng, Luo Ming, Wang Xiangshu, Jia Peimeng
    2014, 35(3):  379-385.  doi:10.11743/ogg20140312
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    Based on the principles of seismic sedimentology and sequence stratigraphy,a high resolution sequence stratigraphy framework was established for the MFS18.5-SB17.5(K set)in Huizhou sag of Pearl River Mouth Basin with 8 sand layers or sand groups recognized.Based on the time-slices of seismic attributes under the constraint of sequence boundary surface,maximum flooding surface and the sub-flooding surface,we studied in detail the seismic facies and sedimentary facies in combination with the well logging and drilling data,cores and regional sedimentary backgrounds.Two depositional systems were recognized in K set of Zhujiang Formation in Huizhou sag,namely the river mouth bar of delta front-sheet sand depositional system in the west,and the shelf ridges system in the southeast.The shelf ridges are characterized by the follows:being located in the front of delta lobes;parallel to the coast in NEE direction,and in stripped distribution;and thinning towards to both edges.Some ridges are thick in one limb and having sharp edges,while the other limb thinning gradually and having irregular edges.This paper discussed the formation mechanism of those striped ridges on the shelf,and pointed out that the striped ridges were resulted from transportation and transformation of delta front sands by waves.And they laterally change into mudstone,thus are important domains for exploration of lighologic reservoirs.

    New understanding of sedimentary facies of Es3(9) in Yi 65 Block of Bonan oilfield at later stage of production
    Gao Buoguo, Xu Fugang, Xu Tao
    2014, 35(3):  386-390.  doi:10.11743/ogg20140313
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    The major pay zone of Yi 65 block in Bonan Oilfield,a low permeability reservoir in production over 30 years,is the 9th sand unit of the 3rd Member of Shahejie Formation(Es3(9)).Nowadays,Yi65 block is at the later production stage.Based on the core,geologic,well logging and production data,we restudied the sedimentary features and microfacies of the major pay zone in the study area.The results show that it is turbidite fan deposit,and can be further divided into three subfacies(inner fan,mid-fan and outer fan)and several microfacies.We described the subfacies and microfacies and mapped the distribution of the sedimentary microfacies of each sublayer.The mid-fan is the main part of the turbidite fan in the study area,and can be further divided into braided channel,inter-braided channel,lateral wing of braided channel and lobes.Reservoirs of the braided channel and lobes are best developed.On plane view,the braided channel occurs in the central part,with the inter-braided channel,lateral wing of braided channel and lower fan occurring successively outwards.The lobes occur at the end of some braided channel.And the briaded channels are of SN-trending or SE-NW-trending.

    Petrologic,geochemical characteristics and origin of the Lower Ordovician dolomite in Yubei area
    Huang Qingyu, Zhang Shaonan, Ye Ning, Li Yingtao
    2014, 35(3):  391-400.  doi:10.11743/ogg20140314
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    The petrologic,geochemical characteristics and origin of the Lower Ordovician dolomite in Yubei area were investigated through the analysis of the cores,thin-sections,SEM,cathode luminescence,trace element,C-O isotope and microthermometry of fluid inclusions.The following results were obtained.Matrix dolomites are of two types:fine crystalline,euhedral-subhedral dolomite and fine to coarse crystalline,anhedral dolomite with saddle fillings.The origin of dolomite is closely related to crystal texture(nonplanar anhedral,planar euhedral/subhedral)instead of crystal size.The fine crystalline,euhedral-subhedral dolomite has high Sr and low Fe-Mn content,and C and O isotope composition similar to that of seawater in Early Ordovician.So this type of dolomite was overall the product of low-temperature dolomitization associated with the Ordovician seawater during the early stage of shallow burial.In contrast,the fine to coarse crystalline,anhedral dolomite has low Sr,relatively high Fe and Mn content and more negative O isotope value.And its fluid inclusion microthermometry result suggests that it has high homogenization temperature and salinity.Combined with the regional tectonic background,it is believed that this type of dolomite was primarily the product of high-temperature dolomitization during late stage of shallow burial to moderate burial,and was locally transformed by hydrothermal fluids from marine-sourced saline water in formation.Moreover,there are two stages of saddle dolomite fillings:one is coeval with the matrix dolomite of hydrothermal dolomitization origin and the other may be associated with the thermal fluid post-magmatic activity during the Permian.

    Sedimentary characteristics of the Cretaceous Denglouku Formation in the southeast uplift of the southern Songliao Basin
    Li Zhandong, Li Yang, Liu Yunli, Hu Huiting, Ma Fengrong, Zhang Xiaogang
    2014, 35(3):  401-409.  doi:10.11743/ogg20140315
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    Sedimentary characteristics and evolution of the Denglouku Formation in the southeast uplift area of southern Songliao basin was studied based on analyses of sedimentary facies distribution and evolution in the context of sequence framework.The results show that the provenance of the Formation were distributed around the basin and supplied sediments from all directions to the center of the basin and the sedimentary facies distribution was controlled by basin tectonic evolution.Five major sedimentary facies were recognized in the area:alluvial fan,fan delta,braided river,braided delta,and lake.The sequence Ⅳ-d1 was formed during the early stage of transformation from a fault depression to a sag.The deposition was mostly controlled by the fault depression and the sediments were downloaded rapidly,restricting the distance of progradation to the inner basin.There developed five separated fault depressions and two small fault depression.Alluvial fan sedimentary systems were developed on the paleohighs around the fault depressions,fan delta systems were located around the fault depressions,while the fronts of the fan delta extended into the mouth of the lake.The sedimentary facies were dominated by alluvial fan,fan delta and lake.Sequence Ⅳ-d2 was formed during the late stage of transformation from fault depression to a sag when an unified sediment unloading area was developed,and the lake expanded.The sedimentary facies were dominated by alluvial fan,fan delta,braided river,braided river delta,littoral and lake.The contact zone of the flood plains and the shore-shallow lake can be regarded as a boundary,to the west of which formed allu-vial fan and braided river systems with sediments sourced from the western and the northern highland provenances;and to the east of which developed retrograded fan deltas of different scales with clastic sediments sourced from highlands.Among the facies,the fan delta front and braided river delta front are considered to be home to hydrocarbon reservoirs and therefore are the most promising exploration targets for oil and gas.

    Sedimentary characteristics and forming conditions of beach-bar sandbodies in the upper fourth member of the Shahejie Formation in the south slope of the Huimin Sag
    Yuan Jing, Liang Huiyuan, Tan Mingyou, Chen Xiaojie, Dong Daotao, Sun Mingjiang, Gao Ruohan
    2014, 35(3):  410-416.  doi:10.11743/ogg20140316
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    Sedimentary characteristics,distribution patterns and forming conditions of beach-bar sandbodies in the upper fourth member of the Eocene Shahejie Formation on the south slope of the Huimin sag have been systematically analyzed in this paper based on detailed core description and analyses of grain sizes,well log,seismic and the regional geological background data.The result indicates that the beach-bar sandstones are dominated by siltstones and fine-grained silty sandstones of high mud content,thus have unfavorable physical properties.Vertically,the beach-bar sandbodies are common in the first sand group but sporadic in the second,the third and the fourth sand groups.Laterally,beach-bars in the studying area distribute along the Xiakou fault.Stable water depth and stronger waves were beneficial to the formation of beach-bar sandbodies.The slope break caused by the Xiakou fault was helpful for beach-bar sandbodies to be formed along the thrown side of the fault but also restricted the horizontal spreading of the beach-bar.Sediments from the basement and earlier deposited layers in flood-overflow lake provided better sediment source for the beach-bar to develop than that from the terminal fan during floo-ding period.

    Quantitative description of intra-platform thin carbonate reservoirs of reef-bank facies and their controlling factors:a case from the A Region of Pearl River Mouth Basin
    Zhang Xiangtao, Wang Xudong, Zhang Sufang, She Qinghua, Ai Jianfeng, Lei Chao
    2014, 35(3):  417-424.  doi:10.11743/ogg20140317
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    Reef-bank carbonate reservoirs is one of the important reservoir types in the petroliferous basins around South China Sea.Proved hydrocarbon reservoirs in A region of the Pearl River Mouth Basin are of reef-bank carbonate type.For a long time,the restriction of the low-resolution of seismic data and poor description of the effective reservoirs have seriously influenced the understanding of the distribution of the reef-bank reservoirs.The integration of various techniques such as frequency-expanding processing,sparse-spike inversion,physical property inversion and the 3D visualization made us successfully reveal the spatial distribution of the reef-bank reservoirs,delineate oil-water contact in combination with drilling data,and calculate the recoverable reserves of the reef-bank reservoirs.The appraisal wells emplaced based on the quantitative description results of the effective reservoirs flowed commercial oil and the drilling results coincide well with the reservoir description,confirming the practicability and effectiveness of the methods.Meanwhile,sedimentary faices belt and fresh water leaching dissolution caused by drops of 4th-order sea level are also closed related with the development of reef-bank reservoirs.In addition,the direction of wind is another major controlling factor on the heterogeneity of reef-bank reservoirs.

    Practice and cognition of shale gas horizontal well fracturing stimulation in Jiaoshiba of Fuling area
    Wang Zhigang
    2014, 35(3):  425-430.  doi:10.11743/ogg20140318
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    The application of advanced fracturing technology greatly increased shale gas production of pilot well group in Jiaoshiba of Fuling area,and improved commercial development of shale gas in China.Based on the analysis of shale reservoir architecture and geological characteristics,the brittleness and fracturability of reservoir rock were evaluated through rock mechanics parameter testing and mineral composition analysis.Shale in Wufeng-Longmaxi Formations is characterized by good organic matter type,high gas content and high brittleness index.According to the idea of "complex fracture network+main supporting fracture",and aiming at enlarging the volume of fractured shale reservoir,we selected most suitable materials for fracturing fluids,optimized fracturing design and related technologies,and determined the technolo-gical methods for fracturing of the pilot well group.Finally,a set of optimal staged fracturing technologies were developed and applied to the horizontal wells in Jiaoshiba of Fuling area.A total of 26 wells were fractured and obtained high open flow of gas in the range of 10.1×104~155.8×104 m3/d,verifying the effectiveness of these fracturing technologies.

    Onset of thermal convection of a viscoelastic fluid in open-top porous media
    Shu Xiaohui, Mu Langfeng, Niu Jun, Ding Jian
    2014, 35(3):  431-434.  doi:10.11743/ogg20140319
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    This paper performed a linear stability analysis for investigating the onset of oscillatory convection of a viscoelastic fluid in an open-top porous medium heated from below.The modified Darcy's law was used to describe the flow of the viscoelastic fluid in porous media and isobaric boundary conditions were introduced to describe the open features The relaxation time and retardation time were introduced to describe the viscoelastic behaviors.Four different combinations of and were selected to calculate the critical Rayleigh numbers corresponding to the onset of thermal convection.The results reveal that the increase of the relaxation time may make it easier to destabilize the flow,leading to an earlier onset of thermal convection.In contrast,the increase of retardation time tends to stabilize the flow and postpone the onset of convection.The flow mode is only related with retardation time.The pattern of temperature disturbance is influenced by the geometric scale of the porous media and the viscoelastic parameters.

    Trilinear flow model and fracture arrangement of volume-fractured horizontal well
    Su Yuliang, Wang Wendong, Zhou Shiyu, Li Xiaohui, Mu Lijun, Lu Mingjing, Sheng Guanglong
    2014, 35(3):  435-440.  doi:10.11743/ogg20140320
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    For low-permeability tight oil/gas reservoirs,economic development is viable only after high-volume hydraulic fracturing which can create multiple fractures and complex network consisting of natural and induced hydraulic fractures.Consequently,fracture arrangement evaluation,prediction of stimulated reservoir volume and well productivity are critical to well stimulation analysis.In combination with the characteristics of tight reservoir and the basics of hydraulic fracture design,we proposed a trillinear flow mathematical model for volume-fractured horizontal wells which can reflect the finite conductivity flow behavior inside hydraulic fractures and massive fractures arrangement.The solution of single fracture at closed boundary condition can be obtained through Laplace transformation.Meanwhile,Stehfest numerical inversion and fracture superposition principle were applied to get formulas of bottom hole pressure and well production for volume-fractured horizontal wells.The model has been valid by using Bakken tight oil production curves.Sensitivity to various para-meters such as fracture arrangement,stimulated reservoir volume,number of fractures have been investigated.The result shows that the pattern of fracture distribution has a great influence on the stimulated reservoir volume;the higher ratio of fracture stage and cluster is,the higher the cumulative oil production of fractured horizontal well is;increasing the numbers of fractures can improve producing efficiency,however,interference between fractures possibly cause the decrease of production.The study results are of great significance for the volume-fracturing design and well productivity evaluation of horizontal wells in tight oil reservoirs.