Loading...
Download
Visited
    Total visitors:
    Visitors of today:
    Now online:

Table of Content

    25 March 1990, Volume 11 Issue 1
    ON THE BASIN TYPE,EVOLUTION FEATURE AND PETROLEUM POTENTIAL OF TARIM BASIN
    Zhang Kai
    1990, 11(1):  1-15.  doi:10.11743/ogg19900101
    Asbtract ( 640 )   PDF (16876KB) ( 463 )  
    Related Articles | Metrics

    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.

    GEOCHEMICAL FEATURE OF CRUDE OLL IN EAST JUNGGAR BASIN
    Wang Yutao, Chen Kexun
    1990, 11(1):  16-22.  doi:10.11743/ogg19900102
    Asbtract ( 704 )   PDF (6102KB) ( 908 )  
    Related Articles | Metrics

    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.

    TECTONIC EVOLUTION OF CHINA SEAS
    Liu Guangding
    1990, 11(1):  23-29.  doi:10.11743/ogg19900103
    Asbtract ( 691 )   PDF (7831KB) ( 429 )  
    Related Articles | Metrics

    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.

    NOTE ON THE CONTINENTAL DEPOSITS OF PENINSULAR THAILAND WITH A DESCRIPITION OF SOME CONCHOSTRACANS
    C. Chonglakmani, W. W. Duan, H. Fontaine
    1990, 11(1):  31-37.  doi:10.11743/ogg19900105
    Asbtract ( 736 )   PDF (5556KB) ( 1106 )  
    Related Articles | Metrics

    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.

    ANALYSIS METHOD AND GEOLOGICAL APPLICATION OF C6+ HYDROCARBONS IN NATURAL GAS OF HIGH EVOLUTION AREAS
    Xu Lian, Qiu Yunyu
    1990, 11(1):  43-50.  doi:10.11743/ogg19900107
    Asbtract ( 620 )   PDF (6444KB) ( 604 )  
    Related Articles | Metrics

    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.

    THE APPLICATION OF STRUCTURAL GEOMETRIC ANALYSIS TO HYDROCARBON PROSPECTING IN EAST SICHUAN
    Dai Tanshen, Ou Zhenzhou, Wang Xu
    1990, 11(1):  51-61.  doi:10.11743/ogg19900108
    Asbtract ( 625 )   PDF (10025KB) ( 374 )  
    Related Articles | Metrics

    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.

    DIAGENESIS OF JURASSIC SANDSTONES IN THE SOUTH MARGIN OF JUNGGAR BASIN,XINJIANG,AND THE PORE EVOLUTION
    Hu Weiyuan, Zhou Jincai, Ma Chuandong, Shi Xuanyu
    1990, 11(1):  62-72.  doi:10.11743/ogg19900109
    Asbtract ( 616 )   PDF (10039KB) ( 403 )  
    Related Articles | Metrics

    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.

    INFLUENCE OF DIABASE INTRUSION ON HYDROCARBON GENERATION OF DEPOSITIONAL ORGANIC MATTER
    Wang Youxiao, Fan Pu, Chen Xuehui, Zhang Qian, Meng Qianxiang, Wang ChunJiang
    1990, 11(1):  73-77.  doi:10.11743/ogg19900110
    Asbtract ( 616 )   PDF (3887KB) ( 898 )  
    Related Articles | Metrics

    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.

    RELATIONS BETWEEN DELTA DEPOSITIONAL SYSTEM OF Es3,SOUTHEAST DONGPU DEPRESSION, AND HYDROCARBON RESOURCES
    Zhu Xiaomin, Xin Quanlin, Fu Shouping, Xia Changhuai, Shi Ruiting
    1990, 11(1):  78-85.  doi:10.11743/ogg19900111
    Asbtract ( 637 )   PDF (8333KB) ( 414 )  
    Related Articles | Metrics

    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.

    STUDY ON LITHOSPHERE TEXTURE OF LONGMEN MOUNTAINS THRUST BELT (CENTRAL-NORTH SECTION) IN SICHUAN PROVINCE
    Liu Shugen, Luo Zhili, Song Hongbiao, Cao Shuheng
    1990, 11(1):  86-95.  doi:10.11743/ogg19900112
    Asbtract ( 658 )   PDF (9160KB) ( 390 )  
    Related Articles | Metrics

    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.

    DISCUSSION ON THE SEDIMENTARY MODEL OF THE MIDDLE TRIASSIC TURBIDITES IN NANPANJIANG BASIN
    Wu Yinglin, Mu Chuanlong
    1990, 11(1):  96-101.  doi:10.11743/ogg19900113
    Asbtract ( 672 )   PDF (5300KB) ( 738 )  
    Related Articles | Metrics

    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.

    STUDING HIGH PRESSURE ANOMALY OF MUDSTONE IN BAISE BASIN BY INTERVAL VELOCITY AND WELL LOGGING DATA
    Li Pengzhen
    1990, 11(1):  102-107.  doi:10.11743/ogg19900114
    Asbtract ( 720 )   PDF (5028KB) ( 398 )  
    Related Articles | Metrics

    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.

    GEOLOGY OF PETROLIFEROUS BASINS AND THEIR SYSTEMATIC ENGINEERING IN RESEARCH
    Zhao Zhongyuan, Liu Chiyang, Ren Zhanli
    1990, 11(1):  108-113.  doi:10.11743/ogg19900116
    Asbtract ( 627 )   PDF (6906KB) ( 454 )  
    Related Articles | Metrics

    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.

    APPLICATION OF LANDSAT PHOTOGRAPHS IN PETROLEUM GEOLOGY
    Ji Yanpeng, He Qingzhi
    1990, 11(1):  114-116.  doi:10.11743/ogg19900118
    Asbtract ( 636 )   PDF (3349KB) ( 363 )  
    Related Articles | Metrics

    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.