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Table of Content

    25 December 1992, Volume 13 Issue 4
    GEOCHEMICAL MODEL OF OIL-GAS GENERATION IN CONTINENTAL FAULTED BASIN
    Zhou Guangjia
    1992, 13(4):  359-370.  doi:10.11743/ogg19920401
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    The basic data about continental oil generation is still the theory on thermal degrada-tion of kerogen commonly used in the world.But during the exploration of hydrocarbon in Jiyang Depression,it was found that the theory should be added and improved.A geo-chemical model of oil-gas generation in two stages—the early and.late stages—has been proposed in this paper.The parent materials to generate oil and gas in the early stage was hydrocarbon polymer parts with low chemical activity contained in some organisms lived in lacustrine basins such as hydrocarbon-rich Botryococcus braunii which containned more than 40% soluble hydrocarbon when cultured living body and generated saturate hydrocarbon series after thermal simulation (R0<0.30%).Two stages of thermal depolymerization and thermal degradation were divided in the late stage.low-matured oil and gas were generated in thermal depolymerization,matured and high-matured oil and gas were generated in thermal degradation.The parent materials of kerogen,favourable for hydrocarbon generation were controlled by biology-rich zones,which would generate the major source beds.As there are much differences in geothermal fields,the source threshold would be controlled by sedimentary units in minor sags.

    SEDIMENTARY FACIES OF QUATERNARY IN PEARL RIVER MOUTH SHELF
    Kou Yangqi
    1992, 13(4):  371-380.  doi:10.11743/ogg19920402
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    According to high resolution geophysical data inthe 3.5 kHz subbottom profile and single-channel seismic reflection,the Quaternary in the Pearl River mouth shelf can be di-vided into four main sedimentary facies and one special deposit body:fluvial facies,deltaic facies,shallow sea facies,tidal current-bayou facies and sand dune-sand wave deposits.These different sedimentary facies are sedimentary systems that formed in low water level,high water level of different periods and transgressive or regressive conditions con-trolled by regional eustasy during Pleistocene-Holocene.

    DISCOVERY OF PALEOZOIC SEDIMENTS IN EAST BAYANHOT BASIN AND ITS TECTONIC SIGNIFICANCE
    Yuan Xiaoqi, Geng Guocang
    1992, 13(4):  381-389.  doi:10.11743/ogg19920403
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    Geophysical and drilling data-proved that Upper Paleozoic sediments of several thou-sand meters thick are preserved in east part of Bayanhot Basin,of which the Ordovician Tremadocian-Arenigian and Llanvirnian-Llandeilian are respectively typical platform de-posits and Helan aulacoge deposits;Carboniferous Tournaisian-Visean and Namurian-Westfalian are respectively steady transgressional deposits and Helan collisional valley de-posits.The discovery shows that the study region had not uplifted all the time.

    RESERVOIR CHARACTERISTICS OF MAJIAGOU FORMATION IN CENTRAL ORDOS BASIN
    Huang Yueming, Yang Yihua, Bao Hongping, Yu Huilong
    1992, 13(4):  390-397.  doi:10.11743/ogg19920404
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    The gas reservoirs of the Majiagou Formation,Lower Ordovician in central Ordos Basin could be divided into four types that are acturally a kind of sabkha composed of gypsum-salt on tidal flat associated with carbonate rocks with clear leaching marks of atmospheric water.

    EVOLUTION OF CRUSTAL STRESS FIELD IN SONGLIAO BASIN DURING HIMALAYA MOVEMENT:EFFECT ON OIL-GAS MIGRATION AND ACCUMULATION
    Qi Lin, Han Guanglin, Zhang Hui
    1992, 13(4):  398-406.  doi:10.11743/ogg19920405
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    Three eposodes of Himalaya movement had considerable appearences in Songliao Basin.The first one happened between Late Tertiary and Early Quaternary.The regional compressive stress of NE-SW direction resulted by the effect of Indian Plate led to the formation of Xiao Hingganling Mountains and the second Songhuajiang-Nenjiang de-pressed zone.The second one took place between Middle and Upper Pleistocene.The com-pressive stress of NW-SE or nearly EW direction resulted by the effect of Pacific Plate led to a large scale of hydrocarbon migration and accumulation,forming a number of anti-cline trapped hydrocarbon pools represented by Daqing placanticline.The third episode in Holocene restored the NE-SW compression that occurred in the first episode,resulting in a series of new hydrocarbon traps or hydrocarbon zones of NW-direction,and seriously reformed the NE-directional anticline trapped hydrocarbon pools.It is suggested that the main target of oil and gas exploration in Songliao Basin is to find new structural traps or hydrocarbon enriched zones of NW-direction.

    GRAIN-SIZE CHARACTERISTICS AND SEDIMENTARY ENVIRONMENT OF CANGFANGGOU GROUP IN BEI SHANTAI AREA,XINJIANG
    Zhao Yongsheng, Zhao Xiafei
    1992, 13(4):  407-417.  doi:10.11743/ogg19920406
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    Clastic rocks of the Permian-Triassic Cangfanggou Group that consist of conglomerate,sandstone,siltstone,muddy siltstone and mudrock are the main reservoir rocks in Bei Shantai area.Based on typical probability curves and their vertical combina-tion,C-M patterns and grain-size parameters combining with sedimentary sequences and their primary structures,log curves,the sedimentary environment of the group is consi-dered as follows:1.alluvial fan including braided stream and fan interval deposition;2.fluvial depositional systems containing meandering stream,low sinuosity stream and in-terfluvial lake;3.delta and lake system.It is suggested that comprehensive analysis of grain-size distribution is a useful tool in sedimentary facies identification.

    RELATION BETWEEN STYLOLITE AND RESERVOIR IN MOXI GASFIELD
    Bai Guilin
    1992, 13(4):  418-422.  doi:10.11743/ogg19920407
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    A study on the types,the property and the distribution of the stylolites in the first submember of Lei-1 member,Moxi Gasfield,and its relation with reservoir show that,the physical property and distribution of reservoir are related to the distribution and deve-lopment of the stylolites;the better the stylolite developed,the thinner the reservoir become,and the worse the physical property.

    EVALUATION OF HYDROCARBON POTENTIAL IN LOCAL STRUCTURES OF HAIAN DEPRESSION:AN APPLICATION EXAMPLE OF FUZZY MATHEMATICAL METHOD
    Xue Bing
    1992, 13(4):  423-430.  doi:10.11743/ogg19920408
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    A method of macro-judgement and micro-judgement in which eight factors including tectonic position,oil-generating condition,reservoir condoition,cap-rock condition,mi-gration and accumulation condition,preservation condition,reliability and seismic stratig-raphy formd the factor set of macro-judgement,and the other six factors containing trap type,trap area,closing height,Percentage of sandstone and mudstone,effective space of reserve,burial depth of the target stratum formed the factor set of micro-judgement was adopted in this paper.It is also introduced concretely how to obtain subordinate functions of every factor and to compose fuzzy judgement matrixes.As the result of judging,36 traps in Haian Depression could be divided into three types.

    RESERVOIR PROPERTY ANALYSIS OF LOWER PALEOZOIC CARBONATE ROCKS IN NORTH CHINA
    Chen Xia
    1992, 13(4):  431-438.  doi:10.11743/ogg19920409
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    Carbonate reservoir rocks of Lower Paleozoic in North China are mainly developed in Middle Ordovician and Lower Cambrian,and are characterized by solution pores and fissures.Karstification and faulting in Caledonian and Yenshan-Himalayan periods resulted in a reservoir zone(200m thick)below erosion surface with dolomite as the prin-cipal reservoir rocks.

    PETROLEUM-GEOLOGICAL FEATURES OF NORTHERN JUNGGAR BASIN
    Liu Quanwen, Bai Guangxia
    1992, 13(4):  439-449.  doi:10.11743/ogg19920410
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    Northern Junggar Basin is a new area for oil and gas exploration.it can be classified as three first-order tectonic units:the Wulungu Depression,the Luliang-Sangequan Uplift and the Central Depression.The main source rocks in these units are the Sangonghe For-mation of the Lower Jurassic,the Baijiantan Formation of the Upper Triassic and the Fongchengcheng Formation of the Lower Permian,and they have reached mature stage.The conditions for the migration,accumulation and preservation of hydrocarbon are favourable in this area.The Shinan Uplift,the north part of the Lunan Depression and the Lunbei faultedfold zone located in favourable position are four prospective oil-gas ac-cumulation zones.Traps ready for drilling recently are the Shinan-3 anticline,Shinan-2 nose,the faulted-nose structure to the north of Lu-4 well and the Yanchi anticline.

    PETROLEUM GEOLOGICAL CHARACTER OF FUXIN BASIN
    Liu Jianying, Wang Shiyun, Yin Jihong
    1992, 13(4):  450-457.  doi:10.11743/ogg19920411
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    Fuxin Basin is a graben-type basin that covers an area of 2000 km2 formed on Pre-cambrian basement during Late Jurassic-Early Cretaceous.Contemporaneous faults could be primarily classified into two groups such as NNE-stretching and NW-stretching faults.The former controlled the thickness and distribution of Upper Jurassic,and the later con-trolled the distribution of coal-rich zones and local structures.The Jiufotang Formation and the third-fourth member of the Shahai Formation are the main source rocks whose organic matter is mainly type-Ⅱ,and the threshold depth of oil-generation that is calcu-lated with average 3.93℃/100m of geothermal gradient is 1350 m.Reservoirs occupy 70% of the total sediment thickness,in which sandbodies of fan-delta and subaqueus gravity-flows are more favourable for hydrocarbon preservation.