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    25 December 1985, Volume 6 Issue 4
    GEOTHERMAL CHARACTERISTICS OF LIAOHE GRABEN
    Wang Ji'an, Wang Jiyang, Wang Yongling, Zhang Zhongyi
    1985, 6(4):  347-358.  doi:10.11743/ogg19850401
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    The prominent feature of regional geotemperature pattern of Liaohe graben is revealed as follows:1.A lower geothermal gradient(about 25℃/km)is inherent for the Ceno-zoic sedimentary strata with a depth shallower than 1,000-1,200m;2.Deeper than that depth,a higher geothermal gradient(35-40℃/km)is observed.This is similar to that of other oil-bearing districts in North China.The intensive circulation of ground water and the structure of the Pre-Cenozoic bedrock are considered as major factores controlling geotemperature pattern in the region studied.Based on temperature measurements of more than 70 wells and hundreds geotemperature data inferred by predictive method recently developed for thisstudy,a set of isotherm maps of different depths has been completed for the whole area with the purpose of specifying the oil-genesis threshold depth,as-sessing oil-gas resources as well as prospecting oil and gas in the district.Heat flow measurements at 54 sites give a mean value of 1.52 HFU(63.6mW/m2)with prevailing value 1.4 to 1.7 HFU.The results are similar to the heat flow measurements in other oil-bearing districts in North China.Suitable geotemperature condition together with aboundant organic ma-terials in Cenozoic sediments,as well as appropriate geological settings and tectonic environment,are considered to be the main factors favorable to the existence of potential oil resources in this area.

    A NOTE ON LONGMENSHAN NAPPE
    Zhao Younian, Lai Xiangfu, Yu Rulong
    1985, 6(4):  359-368.  doi:10.11743/ogg19850403
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    Longmenshan tectonic nappe belt is situated on the northwestern margin of Sichuan Basin,and is approximately 450km long and 40-80km wide,striking in northeast direction.This belt comprises variety of various size of nappes,nappe fragments and slices.These different size tectonic units are separated by diverse over-thrusts,which were developed along tectonically weakened bedding planes in the crust.It is inferred from depth of seismic focuses that the major decollement plane is lying about 17-22km beneath the surface.In addition,some second class of decollement planes are also found at the top of pre-Sinian crystaline basement and within Silurian,Permian and Lower Triassic rocks.The Longmenshan nappe belt was progressively developed from northwestto southeast in close relation with three successive collisions between Indian and Eurasian plates.Namely the mechanics which result in the formation of Long-menshan was exerted from the eastward compressional component of this col-lisions,or it may be presumed that the uplifting of the Qinghai-Tibet plateauand the thickening of the crust that gravity dispersion and the subsequent gravity sliding happened,leads to the formation of series of klippes in thefront of Longmenshan mountains.Typical reverse stratigraphical sequences can be noticed in the domain of this nappe belt.It is suggested that the underlying Sinian to Triassic rocks may contain oiland gas,because they were sedimented in the front of Yangtze para-platform,a condition favourable to oil and gas generation.

    THE TRIASSIC-JURASSIC SEDIMENTARY FACIES OF TARIM BASIN IN RELATION TO TECTONICS
    Gao Xingchen
    1985, 6(4):  369-379.  doi:10.11743/ogg19850404
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    Studies show that the ancient tectonic environment controlled not only the formation and development of Tarim Basin,but also imposed apparent influ-ence on various typical lithofacies of Triassic-Jurassic sediments,for example,the Baicheng and Xinan half-graben depressions,are characterized by narrowlitho facies near the steep escarpments and wide spread lithofacies in shallowslopes;the Tadong downwarping depression is characterized usually by con-centric distribution of lithofacies;while the Minfeng-Jianggesha fault-troughis characterized by symmetrical distribution of lithofacies.On the steeply down-warped side of the half-graben,sediments are predominated by arenaceous-conglomeratic,proluvial and fan-deltaic facies,while on the shallow slope side,they are mainly deltaic,alluvial and shallow water lacustrine facies.Sediments of the fault-trough depression are represented by proluvial and fan-deltaic facies with great number of arenaceous-conglomeratic materials on both sides nearescarpments.Sediments in downwarped region are composed of fine-grained clastics with wide spread deltaic and alluvial facies and a large area of deepwater depocenter.Stratigraphic traps can probably be found in the outer marginof a deltaic structure and tributary channel in the domain of the downwarping region.Traps relative to the proluvial fan-delta might be characterized by fault trough.Whereas in the steeply warped side of the halfgraben,the stratigraphic traps might be discoverd within fan-deltaic and turbidity sediments;while in the gentle slope,traps can mainly develop in the tapering updip sandstones.

    THERMAL EVOLUTION OF ORGANIC MATTERS AND PETROLEUM GENERATION THRESHOLD FOR WELL AICAN-1
    Yang Bin, Ma Qiangmin, Gan Zhanghuai
    1985, 6(4):  380-385.  doi:10.11743/ogg19850406
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    Well Aican-1 is located in the northwest part of Manas depression near the northwestern border of Junggar Basin,with its depth being 5700.13m.The well is ended in the Xiazijie Formation of the Lower Permian.Three suites of source rocks are intersected,i.e.the Lower Jurassic Sangonghe For-mation(J12s),the lower Baijiantan Formation(T31b)of the Upper Triassicand the lower Wu'erhe Formation of the Upper Permian(P21w).Studies of the well temperature,vitrinite reflectance(Ro%),TAI,T-max,S1/(S1+S2),S1/TOC,CPI and 17 steranes and terpanes indices mea-sured by Rock-Eval indicate that the kerogen from the above mentioned for-mations is of humic type,derived in process of thermal evolution.On the basis of this,it is inferred that the threshold depth of oil-generation is about 2,830m,2,830-3,500m at low mature stage,3,500-4,400m at high mature stage,4,400-5,600m at wet gas and condensate stage,and deeper than 5,600m at over-mature stage.

    TILTED FAULT BLOCK-BURIED HILL TRAPS——A NEW TYPE OF OIL/GAS TRAPS IN RIFT-RELATED TENSIONAL BASINS
    Li Desheng
    1985, 6(4):  386-394.  doi:10.11743/ogg19850408
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    Recent ten years or more,a lot of tilted fault block-buried hill oil/gas traps have been discovered by means of geophysical exploration and drilling in the eastern China Meso-Cenozoic rift-related depression basins,the Viking Gra-ben of North Sea of Europe,the Red Sea Graben of Egypt,Sirte Basin of Libya,Gipslend Basin of Australia and the Baffen-Labrador Basin of Canada.High oil/gas yield was recovered from this new type of traps.They are more likely to develop into good exploration targets both at home and abroad.The mechanism of their occurrence can be explained as follows:1.The crust's tensional stress,resulting from the upswelling of the upper mantle,caused a series of tensional rift-subsidence basins,with heat releasedfrom the upper mantle and creating a rather high geotherm-pressure condi-tions.2.The block-faulting break-up of older platforms or basements formed a series of lineally distributed tilted fault block-buried hill structures.3.The rapid subsiding and infilling environments during the early rifting stage were in favorable conditions for maturation and transformation of sourcematerials.Second crop might occur again from the preserved disconformable ol-der source rocks during the later depression stage.4.Suffering from weathering and karstication for a long geological time,the uplift parts of the tilted fault blocks are often good for reservoir forma-tion.5.Combinations of multiple style of traps and multiple source-reservoir-cap assemblages of the rift-subsidence tensional basins could result in multiple-pay pools.

    THE EARLIER PETROLEUM EXPLORATION IN HUABEI BASIN
    Cai Qianzhong
    1985, 6(4):  395-401.  doi:10.11743/ogg19850410
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    In Feb.1955,it was decided in the First National petroleum prospecting Conferencc of the Ministry of Geology that a nation-wide petroleum prospecting sould be carried out.As a result,the Huabei petroleum prospecting Brigade and No.226 Geophysical Exploration Team were set up in the same year,and advanced on Huabei Basin.Since then,large scale prospecting-explorationtasks were carried out in plains and the surrounding mountainous areas in Liaoning,Shandong,Hebei,Henan and Anhui Provinces.At first,main taregt was put on the paleozoic oil and gas,later on,major geological tasks were led to Tertiary System in Jiyang and Huanghuadepressions.Soon afterwards,some subtle structures,such as Dongying,Sheng-licun,Tuozhuang and Yangsanmu structures were discovered.In 1960-1961,the Tertiary dark rock—the Jiyang Group and the Shahejie Formation—favour-able for oil generation,is discovered in wells Boxing-1 and Hua-7,Tertiaryoil sands were also discovered in well Dengqin-3.Based on these inspiring achievements,the Ministry of Geology called together an important stratigicmeeting—Tianjin symposium—in Nov.1960,and resoluted that Jiyang andHuanghua depressions should be taken as the main exploration area and dis-pose correspondent forces.At the same time,the Ministry of Petroleum Industry had also deployed impressive exploration strength and deep drill rigs.Breakthroughs were soon achieved. In 1961,commercial oil flows out from theDongying and Yangsanmu structures,thus laid a foundation for the settingup of Shengli and Dagang oilfields.Later,in 1963,oil flow was drilled atin Fengheying structure in the suburb of Beijing in Jizhong depression.In1964—1965,Lower Tertiary oil sand was drilled at in Huangjindai structurein Xialiaohe depression,and this resulted in the rapid discovery of Liaohe oilfield.In 1973,oil-trace was discovered at last on top of dolomitilized siliceous limestone in the Sinian Wumishan Formation in well Jimen-1 ofRenqiu structure after a lot of failures.In 1975,large amount of commercial oil flows out from well Ren-4 in the Sinian buried-hill within the same structure,thus led to the foundation of Huabei oilfield.

    HYDROCHEMICAL ANOMALY OF NONG'AN STRUCTURE AND ITS SIGNIFICANCE FOR OIL PROSPECTING
    Zhang Jinlai, Wu Dajun
    1985, 6(4):  402-408.  doi:10.11743/ogg19850412
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    The authors have discussed the formation,distribution and properties of hydrochemical anomalies constituted by the concentrations of benzene,me-htyl-benzene,phenol and dissolved hydrocarbon gases in surface water of Nong-an structure,Jilin Province,and the obsorption intensity of the same sur-face water determined by ultraviolet spectrum(260,310nm)and fluorescence spectrum(450nm),in order to guide oil and gas prospecting in the adjacent area.

    CHAROPHYTA ASSEMBLAGES OF TEH CRETACEOUS TO PALEOGENE IN HUNAN PROVINCE
    Hu Jimin, Zeng Demin
    1985, 6(4):  409-417.  doi:10.11743/ogg19850413
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    The charophyte assemblages of the Cretaceous and Paleogene of Hunan Province may be divided into 10 zones(or assemblages)in ascending order.1st zone:Perimneste ancora-Triclypella calcitrapa zone(the middle stageof the Early Cretaceous),represented by the Dongjing Formation of Hengyang Basin.2nd zone:Flabellochara hebeiensis zone(the middle-late stages of the Ear-ly Cretaceous),represented by the Qijiahe Formation of Dongting Basin.3rd zone:Atopochara trivolvis trivolvis zone(the late stage of the EarlyCretaceous),represented by the Mayang Formation of Yuanma Basin.4th zone:Atopochara trivolvis qidongensis zone(the late stage of theEarly Cretaceous),represented represened by the Huitangqiao Formationof Hengyang Basin.5th assemblage:Porochara anluensis-Latochara yuananensis assemblage(themiddle-late stage of the Late Cretaceous),represented by Daijiaping Forma-tion of Hengyang Basin.6th assemblage:Euaclistochara dongtingensis-Maedlerisphaera minuscula as- semblage(the late stage of Late Cretaceous),represented by the YanmatouFormation of Dongting Basin.7th assemblage:Grovesichara changzhouensis-Stephanochara breviovalis as-semblage(the Late Paleocene),represented by the Xinwan Formation of Dongting Basin.8th assemblage:Obtusochara elliptica-Peckichara longa assemblage(the Early Eocene),represented by the Yuanjiang Formation of Dongting Basin.9th assemblage:Obtusochara Jianglingensis-Gyrogona qianjiangica assem-blage(the Middle-Late Eocene),represented by the Hanshou Formation of Dongting Basin.10th assemblage:Maedlerisphaera chinensis-Charites xinhekouensis assem-blage(the Late Eocene-Early Oligocene),represented by the Xinhekou Forma-tion of Dongting Basin.The boundary between the Cretaceous and Paleogene,according to the evo-lution,distribution and property of charophyte assemblages,should be pro-perly placed between the 6th and 7th assemblages.

    THE PALEOCENE SERIES IN EASTERN CHINA
    Yang Runlin
    1985, 6(4):  419-425.  doi:10.11743/ogg19850415
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    The Paleocene Epoch was important in the evolution history of the mam-mal and vice-versa,the later is important to the division of the former.ButCenozoic basins in Eastern China are always rich in microfossils while mammalscould seldom be found,that is why the study of micropaleontological assem-blages has become the key point to the stratigraphic division and correlation.Nanxiong Basin,Guangdong Province,is not only rich in mammal fossils,but also has plentiful microfossils.The Shanghu Formation,as the representa-tive of the Middle-Lower Paleocene,and known in rich Bemalambda assemblage,is associated with ostracods mainly represented by Porpocypris,Parailyocypris taizhouensis and Cypridea with radial sulcus.These ostracods,with some mem-bers of the Parailyocypris make up a transitional type of the Meso-Cenozoic Porpocy-pris-Parailyocypris-Cypridea assemblage;while in the Nongshan Formation,therepresentative of the Upper Paleocene,the extinct Bemalambda are replaced bythe development of Archaeolambda,Phenacolophus and Arclostylops associated with largely breading Sinocypris-Parailyocypris chanzhouensis-Eucypris assemblage of Cenozoic ostracods.The formal transitional to later predominant featuresof ostracods evolution is fit well for that of charophytes and sporo-pollen.Based on the correlation mentioned above,the disputed strata which contain microfossils only are studied in this paper,i.e.the Taizhou Formation of Su-bei Basin,except containing the same micrafossil assemblage as the Shanghu Formation,having more Cypridea fossils with enormous surface varieties,justthe same as charophytcs and sporo-pollen,constitutes a distinctive transitionalzone quite different from that of Cretaceous;the ostracods of the Dalangshan Formation,Sanshui Basin,characterized with the Shanghu and Taizhou For-mations,mainly belongs to transitional assemblage.So it is appropriate to con-sider both the Taizhou and Dalangshan Formations to be the Lower-Middle Paleocene.The 3rd and 4th members of the Funing Formation in Subei Basin,though contain more new species,yet Sinocypris funingensis,S.excelsa,S.multipuncta and Parailyocypris in the strata are all important members of the Nong-shan Formation,they may thus be correlated each other.

    METHANE CARBON ISOTOPE AND ITS APPLICATION IN NATURAL GAS PROSPECTING
    Li Zanhao, Yang Yikang, Fong Minglang, Bu Shuoxun
    1985, 6(4):  426-433.  doi:10.11743/ogg19850416
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    Methane carbon isotopic composition can provide information on origin,maturity and secondary modification of natural gas.Therefore,it can serveas a useful geochemical clue for gas prospecting.The focus of this study isconcentrated on discussing the variation of methane carbon isotope in thermo-genic natural gas.1.It is the temperature that influences the maturity of organic mattersand determines isotopic fractionation range.The fractionation range is largewhen the maturity is lower with methane generated contains light carbonisotopic composition;the isotopic fractionation is decreased,when the methanecontains obviously heavier Carbon isotopic composition.The range of carbonisotopic fractionation depends also on different primary textures of organicmatters,giving rise to methane with its own properties.The isotopic differencein methane and kerogen can manifest the maturity of organic matters.2.The carbon isotopic composition of methane in gas generated from crudeoil become heavier with the increase of cracking of crud oil.The differencein carbon isotope of methane and crude oil can be used to distinguish theoil-cracked gas and the associated one.3.Because of either the emergence of additional gas derived from thelater maturity of organic matters in source rocks or carbon isotopic exchangeunder high temperature,the natural gas affected by high temperature mayproduce an anomalous phenominon of δ13C113C2.4.The manifestation of carbon isotopic composition of methane from coalseams is quite unique,for the less metamorphic coal might bring about ahigher δ13C1 value,while the highly metamorphic coal species might even giverise to lower δ13C1 value.The factor which exercises influence on this valueis more or less complicated.So it can't be used for direct correlation.

    GEOLOGICAL FEATURES OF WANJINTA CO2 FIELD IN SOUTH SONGLIAO BASIN
    Qiu Songyu, Zhong Shiyou
    1985, 6(4):  434-439.  doi:10.11743/ogg19850417
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    Wanjinta CO2 field is located on the western margin of Dehui depression,Songliao Basin.The gas pooled in the Middle Cretaceous Quantou Formation,and is trapped in anticline and stratigraphy-fault-aticline complexities.Thewell yield is more than 20,000m3 of gas per day.The gas comprises 84.5-99.8% of CO2 and a little hydrocarbons.Eachgas pool has its own specific hydrodynamic system.Due to its gravity differ-entiation,the content of hydrocarbon decreases and that of CO2 increases withdepth.The reserve of gas field is quite voluminous and productive.On the ba-sis of δ13C value and regional condition,it is suspected that CO2 was de-rived,and then concentrated,from magmatism.The Early Cretaceous vol-canics to which the Well Wan-5 penetrated more than 939m thick.