最新刊期

    11 1 1990
    • ON THE BASIN TYPE,EVOLUTION FEATURE AND PETROLEUM POTENTIAL OF TARIM BASIN

      Zhang Kai
      Vol. 11, Issue 1, Pages: 1-15(1990) DOI: 10.11743/ogg19900101
      摘要:Tarim Basin is a large,superimposed basin which had a long evolutional history.The evolution can be divided into seven stages,three tectonic cycles of the Proterozoic,Paleozoic and Meso-Cenozioc.Eight prototype basins were superimposed and formed in the central and marginal areas of the basin:Middle Proterozoic-Paleozoic half-graben rift basin,passive continental marginal basin,back-arc fore-land basin,epicontinental sea basin and Meso-Cenozoic back-arc foreland basin,collided foreland basin and reactived collided piedmont basin.Eight hydrocarbon-bearing formations of marine,continental, marine-continental alternative facies(Pt2-Pt3,ε-O,S-D,C-P,T-J,K2-E,N1)were deposited.The basin can be divided into eight structure-depression superim posed regions such as central back arc rift-depressed region,northwest passive continental margin-collided foreland depressed region,north pas-sive continental margin-collided foreland-collided piedmont-collided reactive piedmont depredssed re-gion,northeast passive continental margin-collided foreland depressed region;southeast and southwestback arc foreland-collided piedmont-collided reactived piedmont depressed regions;the collided de-pressed regions of the east and west ends.Four depressed belts,thirteen fault-uplifted and overthrust-folded belts formed in the former six depressed regions.The Tarim Basin is rich in hydrocarbon re-sources and central rift depressed region is especially the first order oil potential area.It is estimatedthat it has the largest potential reserves among the basins in China.In addition,there is geological condi-tion to form inorganic gas reservoirs in the deep of the basin.Five kinds of roof-like,superimposed 3-D hydrocarbon resources are formed in the basin and enriched hydrocarbon zones are as many as 10.These zones are the targets for seaking big,huge even super oil and gas fields.  
      关键词:塔里木盆地;含油气盆地;板块演化;盆地演化;盆地类型;油气聚集带   
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    • GEOCHEMICAL FEATURE OF CRUDE OLL IN EAST JUNGGAR BASIN

      Wang Yutao, Chen Kexun
      Vol. 11, Issue 1, Pages: 16-22(1990) DOI: 10.11743/ogg19900102
      摘要:The authors studied the biomarkers,stable carbon isotope and physical properties of the crude oilin east Jungger Basin and suggested that the crude oil could be divided into three types.Type-A is nor-mal lacustrine crude oil,type-B underwent biedegradation and type-C is coal-formed oil.  
      关键词:准噶尔盆地;原油;生物标记物   
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    • TECTONIC EVOLUTION OF CHINA SEAS

      Liu Guangding
      Vol. 11, Issue 1, Pages: 23-29(1990) DOI: 10.11743/ogg19900103
      摘要:The recongnization of this paper is based upon the geological and geophysical studies of the China seas and their adjacent regions in the past 30 years.The China mainland was developed from some continental cores existing in Pantha lassa and unit-ed as a whole in the Late Paleozoic.The tectonic evolution of the China seas is closely related to the in-teractions among Eurasia,Pacific and Indian oceanic lithosphere plates.It can be divided into 5 stages:1)An ∈,the continental cores formed and developed into blocks or cratons;2)Pz,blocks gradually united as a whole;3)T3-K1,the China mainland was strongly compressed and remaked;4)K2-E2,the margins of plates converged and the interior of the eastern part of Eurasian plate spreaded;5)After E33,the subduction occurred at the margin of Eurasian plate and its interior was widely subsided,and formed today's feature of the China seas.  
      关键词:中国海;大地构造;构造演化;大陆架;海洋地质   
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    • 鄂尔多斯盆地古生界天然气勘探的进展

      王声远, 谢焕功
      Vol. 11, Issue 1, Pages: 30(1990) DOI: 10.11743/ogg19900104
      摘要:鄂尔多斯盆地是一个稳定沉降、扭动明显、坳陷运移的多旋回克拉通盆地。它的早期曾经历寒武、奥陶纪的浅海台地和石炭、二叠纪的近海平原两个发展阶段,分别发育了碳酸盐岩、膏盐和碎屑岩、煤系两大沉积岩系,使古生界具备了丰富的腐泥型裂解气和煤型热解气的资源,为盆地天然气勘探的发展奠定了雄厚的物质基础。  
        
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    • Vol. 11, Issue 1, Pages: 31-37(1990) DOI: 10.11743/ogg19900105
      摘要:After making a study of conchostracan fossils taken from the half way between Trong and Krabi on the southern Thailand of Malaya Penisula,the deposits bearing this fauna are thought to be Middle.Jurassic inage.Thus,it is most probably that there are two conchostracan levels found within Thailand so far.One be-longs to middle Upper Triassic by Kobayashi,and the other is ours of Middle Jurassic.  
      关键词:Thailand;Continental deposits;Biostrata   
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    • 泰国半岛地区陆相沉积评述与叶肢介化石浅析

      C.乔拉克曼尼, 段威武, H.方丹, 彭玉娥
      Vol. 11, Issue 1, Pages: 38-42(1990) DOI: 10.11743/ogg19900106
      摘要:通过对泰国半岛地区董里至甲米之间收集的叶肢介化石的研究,认为含叶肢介化石的地层,其地质年代为中侏罗世。因此,迄今在泰国境内发现的叶肢介层很可能有两个层位,一为小林贞一发现的上三叠统中部,一为我们发现的中侏罗统。  
      关键词:泰国;陆相沉积;生物地层   
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    • Xu Lian, Qiu Yunyu
      Vol. 11, Issue 1, Pages: 43-50(1990) DOI: 10.11743/ogg19900107
      摘要:The authors collected 15 natural gas samples in 4 gas field in Sichuan and identified 71 C6+ hydro-carbons by gas chromatograph.They proposed some new geochemical indices attemptimg to know the conditions of gas generation and preservation.  
      关键词:天然气;天然气中C6+烃类;气相色谱分析   
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    • Dai Tanshen, Ou Zhenzhou, Wang Xu
      Vol. 11, Issue 1, Pages: 51-61(1990) DOI: 10.11743/ogg19900108
      摘要:The fractured gas reservoirs in east Sichuan,no matter they are anticline traped ones or structural fracture pinch traped ones,are all controlled by tectonic deformation.The hydrocarbon enrichment is closely ralated to Himalayan tectonic evolution.The tectonic evolution of the present region in Himalayan orogen has always been disputed,and the division of formation stages differs from each other.Therefore,the evolution in hydrocarbon-bearing structurs may also be different.In application of structural geometric and directional filter analysis,the structures can be divided into four fold sys-tems in this paper according to the folds strikes,the dipping direction of pivots,the closure,cross-sectionpattern,amplitude and depth of folds as well as the configuration on sterographic projection map.Then the evolution of these folds is divided into four generation based on the alternative relationship of big and medium sized folds and the displaced fabric type of the pivots of small sized folds.The distribution and superim position of the fold systems in south,north and central blocks differ greatly from each other due to the control of two northwest strike basement rifts.Through rebuilding tectonic evolution history,the authors consider that,traps formed earlier havethe priority to trap oil and higher enrichment,conversely,the enrichment may low;synclines that up-lifted higher in amplitude and emerged older in strata may have poor preservation condition,otherwise,the condition may good.Exploration in this area has proved that the ratio of success can reach 75% for the wells located according to the above mentioned.  
      关键词:川东;裂缝性油气藏;构造几何分析;定向滤波分析;油气勘探   
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    • Hu Weiyuan, Zhou Jincai, Ma Chuandong, Shi Xuanyu
      Vol. 11, Issue 1, Pages: 62-72(1990) DOI: 10.11743/ogg19900109
      摘要:This paper places emphasis on the diagenesis and its sequence for sandstones of the Lower Jurassic Sangonghe Formation,the Middle Jurassic Xishanyao and Toutun he Formations.On this base,the con-trolling effect and the property of the evolution of porosity by diagenesis are described.The studyshows that the preservative period of valuable pores are the shallow buried stage and deep buried stageafter the formation of secondary pores.  
      关键词:准噶尔盆地;侏罗系;成岩作用;孔隙演化   
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    • Wang Youxiao, Fan Pu, Chen Xuehui, Zhang Qian, Meng Qianxiang, Wang ChunJiang
      Vol. 11, Issue 1, Pages: 73-77(1990) DOI: 10.11743/ogg19900110
      摘要:The authors collected 4 limestone samples and 4 mudstone samples near a diabase body in a basin in Northwest China and analysed the organic matter of the samples.The result indicates that additional geotherm resulted by intrusive mass had evident influence on organic matter evolution.  
      关键词:辉绿岩;异常地热;有机质演化   
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    • Zhu Xiaomin, Xin Quanlin, Fu Shouping, Xia Changhuai, Shi Ruiting
      Vol. 11, Issue 1, Pages: 78-85(1990) DOI: 10.11743/ogg19900111
      摘要:Applying the geological,well-logging and seismic information,this paper studies the basic features of Machang delta depositional system of Es3 in southeast Dongpu Depression.It is considered that Xuji turbidite fan was formed by the slumping of front sediments of Machang delta,thus constituting adelta-slumping turbidite fan system that is connected to each other in origin.The paper also proposedthe target for hydrocarbon prospecting in future based on the analysis of the cause of hydrocarbon en-richment.  
      关键词:东濮凹陷;沙河街组;三角洲沉积;浊积扇   
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    • Liu Shugen, Luo Zhili, Song Hongbiao, Cao Shuheng
      Vol. 11, Issue 1, Pages: 86-95(1990) DOI: 10.11743/ogg19900112
      摘要:According to the processing and analysing of aeromagnetic and gravity data of Longmen Moun-tains thrust belt and its adjacent areas,the magnetic field of this region could be divided into fourzones:Sichuan Basin high magnetic anomaly zone,Longmen Mountains magnetic anomaly steep-chang-ing zone,Pingwu-Lixian negative magnetic anomaly maximum zone,Hongyuan-Maerkang low magne-tic anomaly zone.Regional gravity fields are divided into three zones.The authors pointed out that the one of Longmen Mountains is a positive harmonious anomaly zone.In application of electromagnetic sounding and deep seismic data accosiated with geological analysis,the crust structure horizontally could be divided into four regions(the sima gentle region of west Sichuan Basin,the sima slope region of Longmen Mountains,the sima depressed region of Songpan-Heishui and the sima gentle region of Ruerga-Hongyuan-Aba rigion)and the upper mantle structure into three regions(the mantle gentleslope region of west Sichuan Basin,the mantle steep slope zone of Longmen Mountains and the mantlegentle slope region of Songpan-Ganzi);the lithosphere texture into four layers in vertical(upper crustlayer,lower crust layer,upper mantle cover and the layer underlying the asthenosphere).The paper has revealed the feature of the lithosphere in Longmen Mountains thrust belt and laid afoundation for the studying the mechanism of this thrust belt.  
      关键词:龙门山;逆掩断层带;重力勘探;航磁勘探;岩石圈   
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    • Wu Yinglin, Mu Chuanlong
      Vol. 11, Issue 1, Pages: 96-101(1990) DOI: 10.11743/ogg19900113
      摘要:Turbidity current deposits were developed widely in Nanpanjiang Basin during the Middle Trias-sic.The sedimentary model is submarine fan.This is based mainly on that:1.They have the character-istics of turbidity current deposits.2.They have obvious channel deposits.3.The sequences of the tur-bidity are prograding turbidite fan in the texture profile.The sedimentary model of the turbidity current deposits in the area is not only submarine fan,but several fans with multi-source.  
      关键词:南盘江盆地;三叠系;浊流沉积   
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    • Li Pengzhen
      Vol. 11, Issue 1, Pages: 102-107(1990) DOI: 10.11743/ogg19900114
      摘要:Based on the data of interval velocity,acoustic time difference,gamma-ray log,self-potential,apparent resistivity,caliper log,drilling time etc.,this paper studies the incompact phenomenon of Eogene mudstone in Tiandong Depression,Baise Basin,Guangxi.  
      关键词:百色盆地;泥岩高压异常;层速度;测井   
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    • 皖南海相地层的油气苗

      袁祖华
      Vol. 11, Issue 1, Pages: 107(1990) DOI: 10.11743/ogg19900115
      摘要:皖南地区自震旦纪以来,广泛发育了数千米厚的海相碳酸盐岩,生油岩系厚2000—3600m,生储盖组合配套完整。迄今已在寒武系-下三叠统的各个层段的海相沉积岩中发现不同类型的油气苗数处,其中以泾县北贡、巢县马家山和青阳县木镇的油气苗较引人注目,现作一简略介绍。  
        
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    • Zhao Zhongyuan, Liu Chiyang, Ren Zhanli
      Vol. 11, Issue 1, Pages: 108-113(1990) DOI: 10.11743/ogg19900116
      摘要:Geology of petroliferous basins is a new course proposed by the authors to establish.The present-day research in petroleum geology and the oil and gas prospecting have proved that the sedimentary basins are the foundation units in which oil and gas generate,migrate and accumulate.It has also been proved that to study oil and gas generation,migration,reservoirs,traps,and cap rocks in a basin isolated-ly,and to describe and classify oil and gas accumulation simply can not meet the need of hydrocarbon prospecting.So it is necessary to regard the study of the geology of petroliferous basins as a systematic engineering that all kind of factors are connected with each other.This systematic engineering may be divided into several subsystems as follows:1.Background sys-tem.2.Evolution and deformation system.3.Sedimentary system.4.Hydrodynamic system.5.Thermaisystem.6.Oil and gas system.7.Reformation system.At last,all the achievements in researchof the above subsystems will be synthesized and summarized.Only in this way,the systematic engineer-ing of the petroliferous basins can be a complete system.  
      关键词:含油气盆地;含油气盆地地质学;盆地演化;系统工程;油气资源评价   
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    • 陕北延长组浅油层勘探开发近况

      彭蜀安
      Vol. 11, Issue 1, Pages: 113(1990) DOI: 10.11743/ogg19900117
      摘要:鄂尔多斯盆地陕北斜坡南部三延地区三叠系延长组浅油层勘探开发已有八十多年的历史。80年代前期长庆油田在安塞有新突破,延长组探明储量6500万吨;八十年代后期,又发现南泥湾油田,探明储量达1000万吨,这些油田都与砂体及其成岩作用有关。  
        
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    • APPLICATION OF LANDSAT PHOTOGRAPHS IN PETROLEUM GEOLOGY

      Ji Yanpeng, He Qingzhi
      Vol. 11, Issue 1, Pages: 114-116(1990) DOI: 10.11743/ogg19900118
      摘要:The authores reviewed the achievements they have made in the study of petroleum geology by re-mote sensing.This technique has played animportant role in hydrocarbon exploration in Tarim and oth-er basins.  
      关键词:卫星图象;塔里木盆地   
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    • 地矿部石油地质研究所在开拓中奋进

      朱景善
      Vol. 11, Issue 1, Pages: 117-118(1990) DOI: 10.11743/ogg19900119
      摘要:地质矿产部石油地质研究所于1981年春在北京正式成立。经历九个春秋的艰苦创业,现已初具规模,获得了一批对油气勘查部署有实际意义的科研成果。建所初期,著名石油地质学家朱夏和韩景行高级工程师受命主持所务,呕心沥血,奋斗四载,边筹建、边开展科研,为该所的发展奠定了良好的基础。  
        
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