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    25 December 1989, Volume 10 Issue 4
    RESEARCH AND ASSESSMENT OF CHINA’S PETROLIFEROUS BASINS
    Liu Guangding, Feng Fukai, Wang Tingbin, Xie Qiuyuan
    1989, 10(4):  323-336.  doi:10.11743/ogg19890401
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    China can be divided into five major tectonic areas:North(Siberian- Mongolian)continental margin area,North continent and continentalmargin area,South continent and continental margin area,South(Gond-wana)continent and continental margin area,and East(Peri-Pacific)conti-nental margin area(extensional tectonic system was superimposed after late Mesozoic).These sedimentary basins have two different basinal architectures,i.e.single-layered and multi-layered architectures,each of them forms adifferent basin prototype.Double classification nomenclature can be usedfor those superimposed basins that composed of various basin prototypes.Thebasins in China can be classified into 8 different types,they are:intraconti-nental rift/rift valley,continental marginal rift/rift valley,craton-rift,cra-tonic fold-rift,cratonic rise-fold,intra-orogenic depression,foredeep andcraton-foredeep.The Indosinian tectonic cycle,being a turning point,the evolutional andsedimentary histories of the pre- and post-Indosinian are quite different.Thepre-Indosinian is characterized by steable and widespread cratonic cover,mainly composed of marine carbonate platform deposit,and forms the lowergas-bearing series while the post-Indosinian is mainly comprised of conti-nental clastic sediments deposited in isolated,different sized intracontinentalbasins,which constitute the upper oil- and gas-bearing series.The lower gas-bearing series spread in an area of nearly 300?104km2,in which prolific natural gas has been discovered in Sichuan,Tarim,Ordosand Bohai Gulf basins.The upper oil- and gas-bearing series distribute in anarea of 350?104km2 More than 200 oil and gas fields has been discoveredin the series,constitute over 90% and 60% of our proved oil and gas reservesre spectively.The total petroleum resource in China is 700-1000?108t,of which theresource in the upper series accounts for 60-70%.However,only 10-13% have been proved.Vast vistas is,therefore,still awaiting to be opened up,or rather the upper series will be taken as the main exploration target in aperiod of considerable length.At the same time,of course,a large effort willbe devoted to the exploration of the lower series.The sedimentary basins in China are rather complex.But based on the tec-tonic settings,their oil- and gas-bearing characteristics can be approached by integrating geological,geophysical and geochemical data,and traps andreservoir properties can also be delineated and defined.Thus,taking the ba-sins as a whole,the relational expression proposed by Professor Zhu Xia(1983)can be used to establish computer quantitative dynamic modellingsystem.A thorough study on the sedimentary basins,their petroleum bear-ing regularities and resource assessment can then be made.The resultswould provide scientific basis for exploration deployment.

    DISTRIBUTION OF DICYCLIC SESQUITERPANES AND SEDIMENTARY AND HYDROCARBON-GENERATING CHARACTERISTICS OF RESIN ACID DERIVATIVES IN SALINE-LAKE ENVIRONMENT
    Huang Difan, Zhang Dajiang, Li Jinchao, Huang Xiaoming
    1989, 10(4):  337-345.  doi:10.11743/ogg19890402
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    Using GC/MS technique,the authors studied the dicyclic sesquiterpanes and resin acid-derived tricyclic diterpanes of the Tertiary saline-lake sedi-ments and crude oils in the Qaidam Basin.It is considered that the dicyclic sesquiterpanes may mostly come from pentacyclic triterpanes and the productsof bacteria activity;the input amount of resin derivatives was controlled by salinity of the lake water;hydrocarbon generation of resin acid took placein the early stage of thermal degradation of kerogen.So the hydrocarbon ge-nerated was enriched in low matured oil.

    GEOMETRY OF VITRINITE REFLECTANCE SOLID
    Yang Wenkuan, Ren Chuanhui
    1989, 10(4):  346-354.  doi:10.11743/ogg19890404
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    Vitrinite reflectances may be described by vectors starting from the originof three-dimensional coordinate-system.The length of a reflectance vectordepends on its direction.Theoretically,any vitrinite particle has infinite reflec-tance vectors.These vectors construct a three-dimensional figure called“vitrinitereflectance solid”(VRS).The three principal axes of VRS are maximum ref-lectance Rmax intermediate reflectance Rint and minimum reflectance Rmin res-pectively.The VRS may be double concave,and is not a standard ellipsoidof geometry.This paper deals with the geometrical features of VRS in detail,and provi-des a method for determining the lengths and directions of the principal axesby six readings measured on three mutually perpendicular polished-surface.This method may be used for the studies of petroleum geochemistry,coalpetrology and structural geology.

    PRELIMINARY STUDY ON POSTGLACIAL COASTAL SEQUENCES OF CHINA
    Li Congxian, Chen Gang
    1989, 10(4):  355-365.  doi:10.11743/ogg19890405
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    The postglacial coastal sequences formed during the processes of trans-gression and regression with unconformity at the bottom.Two basic types ofpostglacial sequences in coastal zones of China have been distinguished.Theone in uplift belts consists of superimposed littoral facies,with underlyingbed being bedrocks or old Quaternary beds.The other one was formed indepressed belts,the lower and upper parts of whick are littoral facies with neritic one in between.Terrestrial stiff sand clay of dark green colour thataccumulated during low sea level is the underlying bed.The depressed beltspinched out progressively from coastline to continent,leading to superimposi-tion of lower and upper littoral facies,which then were replaced by terres-trial facies.The storm deposits are well developed in postglacial sequences and showvarious characteristics in different areas and sedimentary units.A few fora-minifera contained in dark green stiff sandy clay are considered as a resultof storm effect.Sand beds with shell fragments and glauconite are storm de-posits and are widely distributed in littoral facies at the northern flank of the Changjiang Delta.In neritic facies of the coastal sequences,the storm depo-sits are represented by sandy gravels with shell fragments in the coastal zones of Beibu(Tonkin)Gulf,and by sand layers that have lower inverse-graded bedding and upper graded bedding in the north flank of the Chang-jiang Delta.In tidal flat deposits of upper littoral facies,there are boulderclay and sand layer of 10-15 cm thick,which are also considered to bestorm deposits.The postglacial sequences in delta areas had been regarded to be conti-nuous without any serious erosion.The study of coastal sequences in deltaareas shows that the coastal sequences developed in ancient valleys and atinterfluve with strong tidal currents,such as Jianggang,often subjected toevident reworking.Only coastal zones where currents are usually weak,se-quences are continuous.

    HETEROGENEITIES AND MODELS OF TIGHT YANGXIN CARBONATE RESERVOIRS IN SOUTH SICHUAN
    Luo Ping, Luo Zhetan
    1989, 10(4):  366-377.  doi:10.11743/ogg19890406
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    Heterogeneous factors that control the paleo-karstification,pressure solution and fracturing of tight Yangxin carbonate reservoirs are explored,and three grades of reservoir models are established in this paper based on geolo-gical data of south Sichuan.The distribution and origin of these special reservoirs such as paleokarst,colluvial breccia and stratiform coral reef areproposed according to Emei taphrogenesis.The main factors leading to the tightness of Yangxin carbonate rocks are pressure solution and cementation,in which the struc tures of the pressure solution can be summarised into 4types and 6 kinds.The development of the fractures in the carbonate rock sunderwent three stages,corres pondingly formed three fracturing reservoir bo-dies such as fracture swarms,dense fracture zones(potential faults)andfaulted breccia zones.In accordance with the distribution and association of the pores,vugs(or cavities)and fractures,the authors have constructed 11potential models of vadose medium reservoirs.These models are proved to beessentially effective in analysing pressure-rebuilding curves and subsurfacegeology of gas field.

    MESOZOIC BASINS IN NORTH CHINA AND THEIR OIL POENTIAL
    Hu Juwen
    1989, 10(4):  378-392.  doi:10.11743/ogg19890407
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    Mesozoic sedimentary basins in North China are mainly single-cycle ones in small or medium size.The formation of the basins underwent multi-stage evolution accociated with volcanic activities and their distribution appears to be in groups and zones.The north and east part of the region uplifted during the Middle Triassic,lacustrine basins that connected to the Ordos Basin formed only in Late Trias-sic in west Henan and south Shanxi.The whole region uplifted in the latestage of Indosinian movement.In the Early and Middle Jurassic,18 basins which were small in size and contained mainly coal scattered in the mobilebelt around the uplift.In Late Jurassic-Early Cretaceous,the depocentcr movedeastward,and the area of deposition extended and dark sequences were well developed.This was the most prosperous period in the evolution history ofthe Mesozoic basins and the basin number was up to 41.Since Late Creta-ceous,basins were not developed well,and only 14 basins left.The sedimentswere generally red clastic rocks.Till now 60 sedimentary basins or residual blocks have been found withinthe area.They can be divided into 6 kinds of proto type basins,i.e.depres-sion,piedmont depression,fold-depression,fault-depression,intermontanefault-depression and fault-depressed volcanic types.They are distributed in 10 regions,west Liaoning,Shijiazhuang-Linqing,Shenqiu,west Henan and Laiyang among these regions are considered to be oil potential areas.

    DISTRIBUTION OF ALKYL-CYCLOHEXANES OF LOWER PALEOZOIC IN NORTHERN MARGIN OF TARIM BASIN
    Zhu Yangming, Zhou Zhongyi
    1989, 10(4):  393-397.  doi:10.11743/ogg19890408
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    Lower Paleozoic sediments in the northern margin of the Tarim Basin con-tain abundant alkyl-cyclohexanes including n-alkyl-cyclohexanes and n-alkyl-methy-cyclohexanes.This article discusses their distribution patterns ofcarbon number.

    CHARACTERISTICS OF STRUCTURAL GEOLOGY AND ITS OIL POTENTIAL IN YANJI BASIN
    Zhang Zhiyi, Gao Pinwen
    1989, 10(4):  398-406.  doi:10.11743/ogg19890409
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    Yanji Basin,located in the east part of Jilin Province with an area of1000km2,is a Meso-Cenozoic basin formed on Hercynian granite and metamorphic rocks during late Indosinian movement.The greatest buried depth of the basement is 3400m.The basin in geotectonic position belongs to Yongji-Aohan fault-folded belt of Tianshan-Xinganling fault-folded System.X-shaped and H-shaped faultsystems controlled the formation and development of the basin.Three first-order structural units can be divided within the basin.Besides,a secondary structural belt—central uplift belt has been discovered by interpretation of landsat photographs and aeromagnetie data.Through the analysis of paleotectonic stress field,the basin is determinedto be stretch origin;the activities of Hegang-Qingjin fault belt have playeda leading role in its formation.The basin contains mainly Cretaceous sediments,then Tertiary depositsand great deal Jurassic volcanic rocks,in which asphalt sandstone,asphalticvein and geochemical exploration abnormality have been found.According to the analysis of the source rock,the authors considered thatsandy shale member of the Lower Cretaceous Dalazi Formation that contains abundant organic matter and is matured has oil forming potential to someextent.So it is inferred that the most favourable place for oil enrichment isthe central uplift belt.

    FORMATION OF OIL POOLS AND HYDROCARBON ENRICHMENT IN DONGPU DEPRESSION
    Wang Xinyun, Xin Maoan
    1989, 10(4):  407-417.  doi:10.11743/ogg19890410
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    The Dongpu Depression(Dongming Depression)crosses Henan and Shan-dong Provinces,The Eogene sediments there are distributed within an area of 5300km2 with a thickness of more than 6000m.Now 15 oilfields have been found.The present article studies the formation conditions of hydrocarbonpools in the depression.

    ON C ARBONIFEROUS HYDROCARBON EXPLORATION IN CENTRAL SICHUAN
    Chen Zongqing
    1989, 10(4):  418-425.  doi:10.11743/ogg19890411
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    The source rocks of discovered Carboniferous gas region both in central andeast Sichuan are underlying Silurian System.Though the thickness and organic abundance of the source rocks in central Sichuan are not as good as that inthe east part,the Ordovician System in central Sichuan is also fine source rock,which may make up a defect for Silurian.The porous bed of the Fucheng-zhai member in central Sichuan—the main reservoir—could be compared withthat of east Sichuan whether in the total thickness or the thickness percentage of the whole member and the weighted mean porosity.The southern part ofcentral Sichuan is in the upper part of a uplift,conditions for hydrocarbon migration and accumulation are no less favourable than that of east Sichuan.In especial,cap and trap conditions are evidently superior to that of the east.In consideration of the above conditions,the author proposed not to domore drilling in the north part,and that the south part should be an impor-tant target for hydrocarbon exploration in central Sichuan.

    PALEOGENE OSTRACODA ASSEMBLAGES AND STRATIGRAPHIC CORRELATION OF THE MAIN DEPOSITIONAL BASINS IN EAST CHINA
    Zhang Shouan
    1989, 10(4):  426-438.  doi:10.11743/ogg19890412
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    This paper deals with palaeontologic characteristics of the main Paleogenedepositional basins in east China.Five assemblages and four evolution phasesof Ostracrda can be summarised.Five fossil assemblages:Upper Oligocene Chinocythere unicuspinata-Dongyingia-Cyprinotus-Cyprois Assemblage.Lower-Middle Oligocene Cyprinotus(Heterocypris)jingheensis-Pinnocypris-Austrocypris-Huabeinia-Chinocythere Assemblage.Upper Eocene Cyprinotus igneus-Echinocypris fabaeformis-Limnocythere jiang-suensis Assemblage.Lower Eocene Sinocypris reticulata-Limnocythere weixianensis-Cypris decaryi Assemblage.Upper Palaeocene Sinocypris funingensis-Eucypris hengyangensis-Parailyocypris changzhouensis Assemblage.Lower Palaeocene Cypridea(Morinina)xindianensis-Porpocypris-Parailyo-cypris taizhouensis Assemblage.Four major evolution phases:1.Meso-Cenozoic mixed fauna phase;2.Sinocypris fauna phase;3.Chinocythere fauna Phase;4.Dongyingia faunaphase.According to the contrast of Ostracod assemblages,a conclusion can bedrawn that the formation of Palaeogene depositional basins took place earlierin South China than in the North.

    SEISMIC-STRATIGRAPHIC DIVISION AND CORRELATION PROJECT OF THE UPPER TRIASSIC SYSTEM IN SICHUAN BASIN
    He Li
    1989, 10(4):  439-446.  doi:10.11743/ogg19890413
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    A seismic-stratigraphic project concerning the Upper Triassic divisionand correlation in central and west Sichuan Basin is proposed in this paperaccording to seismic-stratigraphic method.Based on this project,the authorhas got a new understanding on basin-formation texture,facies distribu-tion,the type and distribution of reservoir sandbodies in the Late Triassic,and also proposed some new targets for oil and gas prospecting.