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    25 June 1989, Volume 10 Issue 2
    STUDY ON THE DELTA DEPOSITION IN FAULT LAKES,YUNNAN PROVINCE,AND ITS SIGNIFICANCE FOR PETROLEUM EXPLORATION
    Zhu Haihong, Yao Bingheng
    1989, 10(2):  95-106.  doi:10.11743/ogg19890201
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    This paper discusses the deposition of fault lakes represented by Dian-chi and Erhai Lakes,the system,feature,facies,distribution model ofdelta deposition,and the significance for petroleum exploration.The research shows that:1.The configuration and water system oflake basin are controlled by tectonic framework.The sizes of deltas areusually small with an area of about 10 to decades km2.The deltas formedalong main fault trend are larger.Therefore,to find deltaic oil-gas pools,we should concentrate our efforts to the ends of elongation direction inthe basin.In a asymmetric basin,median and small sized deltaic oil-gaspools can be found in the gentle slope side.2.Different morphotyped del-tas exist in the same basin.The distribution and evolution of the deltasare controlled by interaction between jet flow of river mouth and longshorecurrent.Main reservoirs are channel sands,river mouth bar sands andfront sheets in fluvial-dominated deltas.The bars that parallel with shore-line are favourable for the formation of oil-gas pools with litho-stratigraphictrap in lacustrine dominated deltas.3.In the early stage of the develop-ment of fault lake or the stage of strong tectonic movement,the sedimentwere eharacterized by debris flow due to the great depth of lake basin waterand steep shore slope.In the latter stage or stable stage,the delta sedimentswere the main type of filling lake basins.In stratigraphic sequences,deltaic oil-gas pools formed in the late stage of every tectonic cycle shouldbe the main objeetives for petroleum exploration.4.The delta sedimentsoften have transitive features between traction current and gravity.The se-diments are composed of the mixture of coarse and fine materials in grainsize and mud content is very high,causing unhomogeneity of sand bodies.Therefore,correspondent method should be adopted to deal with the featuresso as to increase oil production.

    DETERMINATION OF SEDIMENTARY DEPRESSIONS AND PREDICTION OF POTENTIAL AREAS OF COMBUSTIBLE MINERALS OF LOP NUR-ALXA REGION
    Zhang Deyun
    1989, 10(2):  107-112.  doi:10.11743/ogg19890202
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    According to the result of aeromagnetic survey,some sedimentary depres-sions have been determined in Lop Nur-Alxa Region where only preliminarygeological survey is made.The author suggests that Turpan-Hami Depressionetc.are favourable areas for oil and coal exploration.

    GEOLOGICAL STRUCTURES AND HYDROCARBON ENRICHMENT REGULARITY OF GUBEI BURIED HILL IN JIYANG DEPRESSION
    Zhang Rihua, Wang Lichun, Du Xiqin
    1989, 10(2):  113-121.  doi:10.11743/ogg19890203
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    Gubei buried hill,with an area of 60km2 and 1200m thick Paleozoic car-bonite sediments,is situated in the northeast seashore of the Jiyang Depres-sion.5 reverse faults and 2 overturned anticlines have been found here.The formation of the reverse faults and the overtured anticlines wererelated to the sinistral shear-compression of the Tanlu huge fracture andthe obstruction of Chengning uplift.A lot of fissures developed on the top ofthe anticlines due to tensil stress.After long time weathering and erosionfrom the Middle Ordovician to Middle Carboniferous,pores,caves and crevicesdeveloped in the weatherd crust of Ordovician,thus providing favourablespace for hydrocarbon enrichment.Surrounding by source sags,the buried hill has developed into secondaryoil pools with young source beds and old reservoiring beds.Majorproductive bed is the weathering crust of the upper part of the OrdovicianSystem,but the most rich positions are higher levels in the central part ofthe overturned anticlines.

    OIL RESERVOIRS OF LOW OIL-SATURATION IN ALXA REGION
    Yu Jiaren, Tang Jieting
    1989, 10(2):  122-129.  doi:10.11743/ogg19890204
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    In Alxa Region,Eran Basin,oil saturation is as low as 12.5% for andesiteand 23.4% for conglomerate,but pure oil is produced in oiltesting.Theauthors suggest that the productivity of pure oil depends on the oil satura-tion of flowing pore space but not that of availible pore space.

    CONODONTS OF THE TRIASSIC UPPER QINGLONG FORMATION IN DALISHAN SECTION,ZHENJIANG JIANGSU PROVINCE
    Ding Liansheng, Bao Dexian
    1989, 10(2):  130-136.  doi:10.11743/ogg19890205
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    A lot of conodonts are found in Upper Qinglong Formation of LowerTriassic in Dalishan section.They consist of 15 genera and 34 species, and can be divided into two conodont assem blage zones:1.Neospathodus triangularis-N,collisoni A.Z.2.N.homeri-N.anhuinensis A.Z.These correspond to late stage of Olenekian in age,and developed inshallow shelf environment.

    POSITIVE INVERTED STRUCTURES IN SOUTHWEST OF THE EAST CHINA SEA BASIN
    Wang Guochun
    1989, 10(2):  137-144.  doi:10.11743/ogg19890206
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    Geological characteristics in southwest of the East China Sea Basindiffer greatly from those of other parts:1.It was marine environment before the Neogene;2.The faults are distributed in echelon pattern;3.Regional uplift in the end of the Eocene resulted in sedimental lacunaeand erosion for about 15-20 million years in the west part of the area.This article firstly proposed the existance of positive inverted struc-tures.The main proofs are:1.There is a“basin”shape basement beneath the positive invertedstructures;2.Seismic reflection is“dune”shape;3.Sediments of great thickness spread under the structures;4.The fault texture on top of the structures is “flower”shape;5.The faults usually do not cut the basement;6.The upper parts of the structures are generally eroded;7.Formations beneath the structures have abnormal high-pressure;8.Low vilocity.The existance of wrench faults,plastic formations,seesaw motion andhorizontal compression are considered to be the formation factors of thiskind of structures.It has been proved by well drilling in both Bohai and the South ChinaSea that high-pressure mudstones beneath the structures are the most favour-able source rocks.Thus,the structures under which there are plasticformations are favourable places for the enrichment of hydrocarbon in the East China Sea Basin.

    FORMATION AND DISTRIBUTION OF GREEN GRAINS IN THE YANGTSE RIVER MOUTH AREA
    Zhang Guijia, Li Congxian, Ye Zhizheng
    1989, 10(2):  145-153.  doi:10.11743/ogg19890207
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    Green grains in the Yangtse River mouth area can be classified into threegroups:granular,sheet-like and test-mould.The grains are mainly authigenesis in neritic facies.They may occur inother non-marine sedimentary facies such as channel,recent sedimentary areaand sea shore lake basin bog in lower reaches of the river due to the trans-portation of waves,tidal currents and storms.The grains in the relict sedi-mentary areas and in the recent sedimentary areas on the continental shelfare abundant and sheet-like and test-mould particles developed well.The abundances of the green grains in the recent sedimentary areas of the Yangtse River Mouth changes greatly.They may be much higher in deep channels,while much lower in fast-depositing areas where the dynamic condition ismuch weaker.The grains may be carried into typical limnic facies by storm sbut the abundances of those are much lower and the particles are mostly black ovoid.

    CHARACTERISTICS AND SIGNIFICANCE OF EXSUDATINITES IN BROWN COAL OF BAISE BASIN
    Xiong Bo, Zhong Ningning, Wang Tieguan, Huang Guanghui, Zhao Shiqin, Lei Jiajin, Long Wangyin
    1989, 10(2):  154-157.  doi:10.11743/ogg19890208
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    Exsudatinites exist in Tertiary brown coal in Baise Basin,Guangxi Province.According to the data of coal petrology and organic geochemistry,the authors consider that these exsudatinites might be a evidence of hydro-carbon generation and expulsion from immature resinoid.

    DEVELOPMENT CHARACTERISTICS OF THE TRANSITIONAL ZONE IN CENTRALSOUTH SICHUAN
    Xiang Dingpu, Zhang Xiaoping, Wu Dakui
    1989, 10(2):  158-169.  doi:10.11743/ogg19890209
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    The transitional zone in central-south Sichuan is a part of central Sichuan uplift.According to the exploration of a seismic section in this region,there had been tectonic movements between the Lower Cambrian and Middle-Upper Cambrian,the Middle-Upper Cambrian and Lower Ordovician,the Middle-Upper Ordovicion and the Wufeng Formation of the Upper Ordo-vician and the Silurian System as well,with obvious truncation and over-laps.Paleo-uplifts have three patterns in the present region:1.Gradual chang-ing pattern,represented by Caledonian paleo-uplift;2.Sudden changing pattern,represented by Luzhou paleo-uplift of the Indo-Chinese Epoch;3.Over laped uplift pattern resulted by Caledonian and Indo-China Movements.The stratigraphic thickness of Caledonian paleo-uplift differs from thatof Indo-Chinese ones in reverse.The land form during the Caledonian de-posit was high in the west and low in the east,but was reversed during the Variscian-Indo Chinese Epoch.The erosion surfaces of the Caledonian paleo-uplift in the north part of the region and that of the Indo-chinese paleo-uplift in the south may pro-bably form oil and gas pools of weathering crack,monadnock and karst types.

    PRESERVATION CONDITION OF THE LOWER PALEOZOIC NATURAL GAS IN SHANGZHI-SHIMEN SYNCLINORE,NORTHWEST HUNAN
    Ying Weihua, Huang Lianghan
    1989, 10(2):  170-181.  doi:10.11743/ogg19890210
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    Shangzhi-Shimen Region,with a total area of about 10000km2,is situ-ated at the northwest margin of the Jiangnan Old Land.The basic struc-tural type is two depressions in the north and south and a uplift in be-tween.Start from north to south,it is composed of Taiqing shan-Hongjiaguan syncline zone,Siwangshan-Huangchang anticline zone and Dayong-Shimen syncline zone.The source beds are the Lower Silurian,Or dovician,Lower Cambrian,the Dengying and Doushantuo Formations of the Upper Sinian,the mainre servoir is the Dengying Formation.The fractures in this region are characterized by well developed combinedstriks of different directions and multi-stage activities.They are usually filled by low-temperature hydrothermal deposits,some of them have ther-mal springs accociated with nitrogen.All this may be harmfull to hydro-carbon preservation.The preservation condition of Siwangshan-Huangchang anticline zone is better,Yanzhiyan anticline,a part of the anticline zone,formed earlier than others and has favourable trap condition.

    PETROLEUM-GEOLOGICAL IMPLICATION OF SATELLITE PHOTOGRAPHS FROM YINING REGION
    Wang Xiuqian
    1989, 10(2):  182-188.  doi:10.11743/ogg19890211
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    The author made a interpretation for the satellite photographs from Yi-ning Region,Xingjiang Uygur Autonomous Region,and pointed out 4possible regions of hydrocarbon enrichment.

    DEPOSITIONAL CHARACTERS OF THE CARBONIFEROUS PERMIAN LIMESTONE IN SOUTHEAST SHANXI
    Xiao Wuquan
    1989, 10(2):  189-194.  doi:10.11743/ogg19890212
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    Coal-bearing strata in southeast Shanxi consist of carbonate rocks (lime-stone,clastic rocks and coal.According to macroscopic and microscopic study,the author suggests that the limestone developed in intertidal to the upperpart of subtidal zone of the freshening bay.Sea water repeatedly floodedoff shore marshes and ponds of mud banks due to tidal and storm,resultin in this unique coal-limestone assemblage.