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    25 June 1984, Volume 5 Issue 2
    OVERTHRUST BELTS ON THE NORTHERN MARGIN OF QAIDAM BASIN AND THEIR OIL PROSPECTING
    Di Hengshu
    1984, 5(2):  79-88.  doi:10.11743/ogg19840201
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    A group of huge faults overthrusting from north to south along the southern sides of Mts.Saishiteng,Luliang,Xitie and Aimnik cn the northern margin of Qaidam Basin are found in outcrops with dip angles of seventy degree or more,but seismic data available show that the dip angles of these fault planes in the lower part of Tertiary are gradually reduced and finally turned to twen-ty or lesser within Prepaleozoic sediments.Another huge fault,Maxian fault,overthrusting from south to north is located at the north side of Mahai and Nanbaxian anticlines on the southern margin of eastern Saishiteng depression with a dip angle of thirty degree.Between these opposite dipping faults,there lays Mahai-Pingtan depression with sediments of Meso-Cenozoic system which measures to 10,000m or more in thickness,among them,more than 1,200 mthick sediments belong to Mesozoic,in which the 5th and 7th members of the Dameigou Formation of Middle Jurassic,the source rock in this area,might be existed and covering a area of about 1,500km2.Within this depression,some petroleum fields have been found out,e.g.western Yuka Oilfield with Upper Jurassic pay zone is in the north,and Mahai Gasfield with Oligocene reservoir in the south.It is proved by seismic prospecting that the concealed Mahai-Pingtan anticli-nal nose has a trap area of 176km2 in upper Mesozoic,and supposedly,other traps might exist somewhere eastward.These subtle traps,together with Mahai and Nanbaxian anticlines,might respectively belong to the footwall and hanging wall of the Maxian fault.This area,being close to the petroleum generating depression,having good traps,is therefore favorable for oil prospecting.In western Saishiteng depression,there are a series of concealed anticlines along the footwalls of Tuonan and Quenan faults.The 5th member of the Dameigou Formation,the source rock of Lenghu Oilfield,may distribute in this region,which could be 1,000-1,300m thick,and is potential for oil gene-ration,and as it is near the Lenghu 4th and 5th Oilfields with Tertiary reservoir and Lenghu 3rd Oilfield with Jurassic pay bed,this area is also very hopeful in petroleum exploration.

    RELATIONSHIP OF OIL AND GAS WITH VOLCANISM IN SANSHUI BASIN
    Tang Zhongyu
    1984, 5(2):  89-100.  doi:10.11743/ogg19840202
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    The Eogene volcanism were quite often in Sanshui Basin.Various lavas and volcanic clastics,totalling about 2,000m thick,were formed in more than one hundred times of volcanic eruption.They distribute mainly in the central part of the basin which measures 45 km long NS and 8-12 km wide EW,and formed in the process of deposition of the Buxin Formation(E1-2b),the source rock,and also in the generation and migration process of oil and gas in it.As a result,they have exerted great influence both on the accumulation and preserva-tion of oil and gas.The high ancient geotherm derived from the volcanism had accelerated the evolution of source rocks,so the depth of oil generating threshold is 800-1,200mshallower than that in basins elsewhere in the eastern part of China.The abundance of organic matters,such as organic carbon,chloroform asphalt and hydrocarbon,decreased remarkably due to volcanism within this area,resulting in poor oil and gas showing.Rocks rich in organic matters are distributed in a horse-shoe belt surrounding the centre of volcanics,showing clear relationship to the distance away from the area of volcanic eruption centres or subvolcanic intrusions and also to the shape and volume of lavas.In fact,almost all oil and gas fields and wells with good showings are located around the area of volcanic activities.Volcanism occurred during the stage of oii and gas migra-tion,for example,formed in the deposition process of the Huayong Formation (E2-3b),had brought serious damage to oil and gas.Diapiric and draping structures were formed due to volcanic activities in San-shui Basin,but they bear no significance for oil and gas accumulation,because of their delay in formation.The highly pure carbon dioxide(99.5%)pools discovered in the present area are closely related to volcanism,they distribute in or close to the terrain of volcanic rocks.

    TERTIARY STRATIGRAPHY OF ZHUJIANGKOU BASIN
    Duan Weiwu, Lei Zuoqi
    1984, 5(2):  102-112.  doi:10.11743/ogg19840203
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    The Cenozoic sediments in Zhujiangkou Basin disclosed in 7 offshore wells are dominated by clastic rocks with intercalations of combustible organic deposits in its lower and middle parts,the maximun thickness totals 3,350m.Ac-cording to the lithological characters and microfossils they contain,the Tertiarysediments can be divided into six stratigraphical units,in ascending order,theyare the Baoan Formation,Zhuhai Formation,Zhujiang Formation,Hanjiang Formation,Yuehai Formation and Wanshan Formation.The Baoan Formation and Zhuhai Formaton are characterized by abundant sporopollen,which may be distingushed into Taxodiaceaepollenites-Gothanipollis and Ostryoipollenites-Pinuspollenites assemblages aged to Oligocene.The Lower Miocene Zhujiang Formation contains calcareous nanofossils belonging to Sphenolithus belemnos zone and Helicosphaera ampliaperta zone,and Foraminifera of Globoro-talia jiaweiensis-Cassigerinella chipolensis assemblage.The calcareous nanofossils recovered in the Middle Miocene Hanjiang Formation are members of Triquetror-habdulus rugosus zone and Catinaster coalitus zone,which occur along with Foraminifera of Turborotalia siakensis zone.Abundant sporo-pollens belonging to two assemblages are also recovered in the Hanjing Formation,namely(in ascending order):Florschuetzia trilobata-F,semilobata,F.levipoli-Zonocostites of.ramonae.The Upper Miocene Yuehai Formation is characterized dominantly by coarse clastics,containing nanofossils of Discoaster quinqueramus zone and Amaurolithus amplificus zone,and Foraminifera of Ammonia altispira(nearshore) or Globigerina nepenthes zone(offshore). The nanofossils in the Pliocene Wanshan Formation are mainly preserved inits mid-lower parts,represented by Sphenolithus abies zone and Discoaster tamaliszone.The simultaneous Foraminifera is characterized by Globorotalia multicamerata-Sphaeroidinellopsis seminulina assemblage.Owing to regression,the upper part of the Wanshan Formation lacks calcareous nanofossils,but the benthic Foraminifera and Ostracoda are well developed.

    BITUMEN GENERATION POTENTIAL OF KEROGEN
    Yang Wenkuan
    1984, 5(2):  113-121.  doi:10.11743/ogg19840204
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    Methods for estimating the bitumen and the methane generation potentials of kerogen are proposed in this paper.The problem of estimating the initial abundance of kerogen according to the abundance value of organic carbon is also discussed.It is worth noting that,in these methods,not only the changes of atomic ratio of kerogen have taken into account,but also the TGA weight loss of kerogen has considered.The bitumen generation potential means the maximum capacity of kerogento yield liquid bitumen plus gaseous hydrocarbon.As for the types Ⅰ,Ⅱ,andⅢ of kerogen being at the threshold of petroleum generation,their bitumen ge-neration potentials are about 61%,43% and 6% respectively.The methane generation potential means the weight ratio of the methane versus the initial kerogen generated after complete degradation of the latter,with res-pect to the types Ⅰ,Ⅱ and Ⅲ of kerogen being at the threshold of petroleum generation,the methane generation potentials are respectively about 35%,25% and 6%.For a close system of petroleum generation,after complete degradation of kerogen,residual solid carbon abundance being multified by factors of 1.42,1.30 and 1.09 may correspond respectively to the carbon abundance of the kerogen types of Ⅰ,Ⅱ and Ⅲ being at the threshold of petroleum generation. While for a open system,factors to be multified are 2.66,1.83 and 1.10 res-pectively.

    CHARACTERISTICS OF RESERVOIR ROCKS AND THEIR DIAGENETIC EVOLUTION IN THE NORTHERN PART OF SONGLIAO BASIN
    Du Bomin, Xing Shunquan, Zhou Shuxin
    1984, 5(2):  122-131.  doi:10.11743/ogg19840205
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    Sedimentary characteristics and diagenetic evolution of reservoir rocks in the northern part of Songliao Basin are discussed here,taking the sandstone of Da-qing Oilfield as an example.They are represented mainly by terrigeneous coarse siltstone and fine-grained sandstone,mostly belong to detrital feldsparthic sand-stone and greywacke.The physical properties containing oil constrained essen-tially by sedimentary and diagenetic conditions vary greatly,they are getting worse mainly with the buried depth of reservoir,having little affects by its lithologic character.The most favourable reservoir rocks are the upper and middle oil-bearing assemblages buried above the depth of 1,500 m,including Heidimiao,Saertu,utaohua and Gaotaizi pay zones,the lower pay zones,buried within the depth of 1,500-2,000m or 1,500-2,500m such as Fuyu and Yangdachengzi zones,arefairly favorable;the still deeper strata below 2,000m or 2,500m depth,e.i.sandstones beneath the second member of the Quantou Formation,are considered as posble gas-bearing zones.The primary porosity and permeability of sandstones were constrained by sedimentation,while those of secondary origin were largely constrianed by diagenetic conditions.Common authigenic minerals in this area consist mainly of quartz,feldspar,montmorillonite,kaolinite,illite,chlorite and other tran-sitional phases of clay,with small amount of calcite,siderite and glauconite.They were formed during diagenesis from chemical consolidation.Special attention have been attached to attributes of authigenic assemblages and their mode of occurrence in this study in order to estimate their influence on physical properties of reservoir,and therefore,to predict the possible damage which might occur during oil production.

    DISTRIBUTION AND FORMATION OF SALTS AND THEIR RELATIONSHIP WITH PETROLEUM GENERATION IN QAIDAM BASIN
    Sun Dapeng
    1984, 5(2):  132-139.  doi:10.11743/ogg19840206
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    Qaidam Basin,ever developed with sulphate water,is typical in salts and petroleum coexisting continental lacustrine basins.Various kinds of salts,such as gypsum,halite,mirabilite,bloedite,epsomite,potash,bischofite,borate and celestite are found in Qaidam Basin,mainly distributed in Pliocene to Holocene series.Salt formation could be divided into two stages,i.e.the first,Pliocene to early and middle Pleistocene,and the second,late Pleistocene to Holocene.The former mainly occurred in the western part of the basin,sulphate waters of which were precipitated typically in continental environment;the later is proceeding in all the modern saline lakes of the Qaidam Basin,the western part of which contain sulphate waters,while those in the eastern part contain chlorate waters.It is assumed that the salt precipitaton was proceeded after vigorous uplift ofthe present region,under dry climate,and by ways of different crystallization process and salt separating sequence for different types of waters.Therefore,two salt-formation patterns have been suggested:the"tear drop"pattern and the "bull's eye"pattern.The former is important not only for the formation of salt,but also for oil and gas.The major oil source rocks are in Oligocene and Miocene in the western part of the basin,while main gas source rocks are in the middle-lower Pleistocene in its eastern part.They were formed in deep lacustrine lakes,where slightly saline to simi-saline sulphate waters under the more humid climate while the region suffering stable downwarping.According to spacial and temporal relationship between the formation of salt as well as oil and gas,three patterns can be suggested:1.Typically,oil and gas are formed before the salt precipitation;2.Oil(-gas)and salt are formed at the same time,but not at the same place;3.Salt and oil-gas are formed alternately.

    ON THE OPTICAL PROPERTIES OF KEROGEN
    Wen Suqiu, Wang Peihong
    1984, 5(2):  140-147.  doi:10.11743/ogg19840207
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    Shape,colour,transparency,structures and fluorescene of kerogen mainly from lower Crataceous Qingshankou Formation are studied with microscope under transmission light,reflected light and polarized light in conjunction with fluorescene and electronic scanning microscope.Kerogen is divided according to these optical properties into sapropelized,stablized,gelled and fusited mace-rals,and three major groups of kerogen,such as sapropel type,mixed type and humut type,are made relative to proportion of each component.On the basis of this study,it is identified that the kerogen from the Qingshankou Formation is mainly of sapropel type in the stage of maturity or nearly maturity.Although the type of kerogen could hardly be distinguished by means of chemical method for samples from outcrop or highly evolved one,yet it can be detected on the basis of their optical attributes.

    ON THE MIOCENE SEDIMENTARY ENVIRONMENT IN WESTERN TARIM BASIN IN VIEW OF MICROFOSSIL ASSEMBLAGES
    Yang Runlin
    1984, 5(2):  148-155.  doi:10.11743/ogg19840208
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    In western part of Tarim Basin,the Miocene is represented by a sequence of clastic sediments which can be divided in ascending order into three forma-tions:the Kezilouyi,Anjuan and Pakabulake Formations.The Kezilouyi andAnjuan Formations are composed of continental sediments deposited on a Paleo-gene erosion surface or abandoned lagoonal basin,containing a few of continen-tal Ostracoda and Charophyta.The 3rd to 5th members of the Anjuan Formationare characterized by abundant Cyprideis and Ammonia,with some horizonscontaining Ostracoda and Charophyta common to continental fresh water,suggesting a transitional facies.According to the variation of microfossils,12 sedimental environments of the Anjuan Formation are recorded.Five ofthem are transgressional,represented by fine-grained sediments,well-developedmarine fossils,enriched salinity;while those of regression horizons arerepresented by retired lacustrine basin,coarse-grained sediments,decreasedsalinity and appearance of fresh water fossils.All the ransgressive horizons are rich in organic matters,have higher rate of deposition and plenty of darkargillites with larger thickness of single bed.They are mainly distributed in Wuqia region,totalling about 200m thick.Organic matters are not quite developed in abnormal continental sediments,but they occupy large areas.The Pakabulak Formation comprises entirely clastic sediments.

    MULTIVARIATE STATISTICAL METHOD APPLIED IN STUDYING SEDIMENTARY ORGANIC MATTERS OF OLIGOCENE IN JIYANG DEPRESSION
    Zhou Guangjia, Yan Hanjie, Yan Huarong, Mao Jinbiao
    1984, 5(2):  156-167.  doi:10.11743/ogg19840209
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    14 specimens of representative immature source rocks of Oligocene from Jiyang depression in Shandong Province and 16 samples of peat soil and muck from Jilin,the East China Sea,the Bohai Bay,Weishan Lake and Futong River are studied through factor analyses,including R-type and Q-type analyses,and correlative analyses on the basis of 28 geochemical indexs,to identify the correlativity among samples and/or indexes. Results of this study show that the organic matters of Oligocene in Jiyang depression have the characteristic of near-shore fault-block bounded lacustrine basin with continental organic matters mixed with a little marine organic mat-ters.It has been proved that when this type of organic matters reaches sufficiently enough quantity in a matured environment,commercial oil and gas may be generated.

    A PRELIMINARY STUDY ON THE MECHANIC PROPERTIES OF CONCEALED FAULTS WITH INFORMATION OF ACOUSTIC LOGGING
    Liu Zerong, Chu Zehan, Wu Nailing
    1984, 5(2):  168-178.  doi:10.11743/ogg19840210
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    The mechanical properties of four faults concealed by loose Quarternary deposits in Shengli Oilfield are studied with the information of acoustic log-ging in the light of principals of mechanism geology.Various characteristics of time difference anomaly have been traced in faults of different mechanical properties,a new method for identifying them is simultaneously turned out in this paper.It is proved in the living example researched that tectonites within compresive fault belt give rise to a clearly smaller time difference of acousticwave than those of lithologically the simillar non-tectonites,that is to say,a faster acoustic velocity is transmitted by the former;on the contrary,a lar-ger time difference of acoustic wave have recorded in tectonites within tensionalfault belts,i.e.the acoustic velocity within these belts is lower.

    ALCYONACEA-SPICULA LIMESTONE IN HAINAN ISLAND
    Wang Shuyi, Huang Hengquan
    1984, 5(2):  179-182.  doi:10.11743/ogg19840211
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    Recent carbonate sediments were formed about 4,000-5,000 years ago in Shuiweiling and Ximao Island,Yaxian County,which consist simply of Alcyona-cea spicula.All nodes and spines are well preserved on the surfaces of these spi-cula,and no sign of transporting abrasion can be observed.They are just thesame as the alive ones both in shape and structure,but mineralogically they arequite different,making up mainly of low-Mg calcite with MgCO3 content rang-ing from 1.9 to 4.9 mole%.The cement consists predominantly also of low-Mg calcite,which occurs in fibrous rims,micritized equant grains.These fabricforms and relic composition indicate that the primary mineral of the cement should be high-Mg calcite or arragonite formed in marine diagenetic environment.The isometric-granular calcite might be formed in a zone of underflow of fresh water,judging from its lacking cresecent and pendant forms of petrofabric which are characteristic in seepage zone.This spicula limestone was formed due to decomposition of sof issues of Alcyonacea and their consequent washout.However,the washing out should not occur before the burying because if it did,this might result in the scattering of these spicula,the contamination by impurities and the subjecting to abrasion.The later uplift of Hainan Island probably brought the approximatly cemented Alcyonacea-spicula limestone into an freshwater underflow environment,which made it subjecting further to consolidation and modification.

    THE EXPLORATION AND EXPLOITATION OF NATURAL GAS IN SICHUAN BEFORE THE QING DYNASTY
    Chen Shi
    1984, 5(2):  183-192.  doi:10.11743/ogg19840212
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    China is one of the earliest countries in discovering and using natural gas resource in the world.The great achievements made by both the ancient and modern Sichuan people in natural gas geology,and technology in drilling,exploitationand transportation,etc,rather collectively show an outline of the historical deve-lopment of the tremendous contributions of China.After studing a great deal of his-torical literatures from the Han Dynasty to the end of the Qing Dynasty,and therecent reports of geological exploration,the author tries hard to study systema-tically this long historic process.Namely,the writer has firstly collected and analysed a lot of documents related to the first gas well—Linqiong gas well—in theworld;secondly,introduced the situation of the early use of the natural gas in Si-chuan;thirdly,expounded the exploration and exploitation courses of gas resourcesin Ziliujing saltfield from 16th to 19th century A.D.as well as the construc-tion process of this earliest natural gas production ase in the world;the fourth,emphasised discussion on the experience and working manner in locating wells,identifying lithology,making geological logging and tracing fractures of the pioners who had properly treated the geological task of natural gas;and finally,the author gives a brief review of the three stages in the development of drilling techno logy and the characters of the technology about exploitation and transportation.

    REVIEW OF PETROLEUM GEOLOGY OF CHINA
    Gan Kewen
    1984, 5(2):  193-194.  doi:10.11743/ogg19840213
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    The book Petroleum Geology of China,edited by Professor Wang Shangwen,is divided into 4 parts and 10 chapters,containing about 350 pictures,500 thousand words and covering 343 pages.Part one:China's tectonic outline and the division of oil-and gas-bearingareas;Part two:Genesis of hydrocarbon and source rocks in China;Part three:The migration of hydrocarbon as well as oil and gas pools inChina;Part four:China's oil-and gas-bearing basins and the distribution regulari-ties of hydrocarbon.