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《Journal of Palaeogeography》 2008-02
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Discussion on relationship between sedimentary evolution of the Triassic Yanchang Formation and the Early Indosinian Movement in Ordos Basin

Deng Xiuqin Lin Fangxiao Liu Xianyang Pang Jinlian Lü Jianwen Li Shixiang Liu Xin Research Institute of Exploration and Development,PetroChina Changqing Oilfield Company,Xi'an 710021,Shaanxi  
The sedimentary characteristics of the lower part of the Yanchang Formation(Chang 10—Chang 8 oil bearing intervals)are quite different from the middle and upper parts of the Yanchang Formation(Chang 7—Chang 1 oil bearing intervals).During the deposition of the lower part of the Yanchang Formation,the western and southwestern areas of the basin were characterized by a gentle topography and the deposition was dominated by the braided fluvial,braided fluvial deltaic and coastal-shallow lacustrine facies.The content of chemically unstable components was relatively higher in clastic rocks.The depositional framework changed greatly during the deposition of Chang 7 interval of the Yanchang Formation.The sedimentary systems changed to alluvial fan and fan delta in the west and southwest.The size of the downwarping depression increased quickly and semi-deep and deep lakes covered an area of over 10×104 km2.Simultaneously,the depocenter of the Ordos Basin was shifted tens of kilometers southwestwards.The component maturity of the clastic rocks increased and the rock combination was obviously different in the west and east dispersal tracts of sediments.Furthermore,analyses of the distribution of the tuffs in the Yanchang Formation indicate that the tuffs are steadily distributed in the basal part of Chang 7 interval of the Yanchang Formation and they were derived from the syn-depositional volcanism.Their thickness decreased from the southwest to the northeast.These analyses indicate that the latest depositional period of Chang 8 interval of the Yanchang Formation is an important transitional stage in the basin's sedimentary evolution.A strong tectonic movement occurred in the western margin and southwestern margin of the basin and volcanic activities took place frequently.These events represent the first episode of the Indosinian Movement.
【CateGory Index】: P512.2
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1 LIU Shao-peng~(1,2),ZHOU Shi-xin~1,WANG Bao-zhong~(1,2),LI Jing~(1,2),ZHANG Hai-kun~(1,2),GONG Shu-hua~(1,2) (1.Key Laboratory of Petroleum Resources Research,Institute of Geology and Geophysics, Chinese Academy of Sciences,Lanzhou 730000,China; 2.Graduate University of Chinese Academy of Sciences,Beijing 100049,China);Relationship between Industrial Indexes and Source Rock Evaluation Parameters of Oil Shale[A];[C];2013
2 ZHANG Xiao-li~(1,2),DUAN Yi~1,HE Jin-xian~(1,2),WU Bao-xiang~1,XU Li~(1,2) (1.Key Laboratory of Petroleum Research of Institute of Geology and Geophysics, Chinese Academy of Sciences,Lanzhou 730000;2.Graduate School, Chinese Academy of Sciences,Beijing 100049,China);Characteristics of the Sedimentary Microfacies and the Oil and Gas Distribution of Chang 2 Reservoir of Yanchang Formation in Linzhen Area,Ordos Basin[A];[C];2013
【Secondary Citations】
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1 He Qixiang ( Institute of Marine Geology, Qingdao ) Liu Zhaojun Wang Dongpo Hu Zhenguo Liu Wanzhu ( Changchun College of Geology );CHARACTERISTICS OF LACUSTRINE TURBIDITES AND THEIR TECTONIC SIGNIFICANCE[J];Acta Sedimentologica Sinica;1984-04
2 Ke Baojia Chen Changming (Institute of Geology, Chinese Academy of Sciences) Jiang Haoren Hui Binyao (Institute of Petroleum Exploration and Exploitation, Changqing Petroleum Bureau);Sedimentology of Gravelly Alluvial Fans on the Western Margin of Late Triassic, Ordos Basin[J];Acta Sedimentologica Sinica;1991-03
3 Mei Zhichao I'm Jinyan (Department of Geology, North an);Stratigraphic Pattern and Character of Skeletal Sand Bodies in Lacustrine Deltas[J];Acta Sedimentologica Sinica;1991-04
4 Jiao Yangquan; Zhou Haimin; Zhuang Xinguo; Liu Shaofeng; Yang Shengke; Ma Meiyuan(China University of Geosciences, Wuhan 430074)(East Hebei Petroleum Exploration and Development Company,Hebei Tangshan 063200);Fan Deltaic Depositional Systems and Their Relationship to Oil and Gas Accumulation[J];ACTA SEDIMENTOLOGICA SINICA;1998-01
5 WEI Hong hong 1 PENG Hui qun 2 LI Jing qun 2 XIE Zheng wen 2 QI Diao liang 2 1 (Department of Geology Northwest University Xi ’an 710069) 2 (Workover Company Changqing Bureau of Petroleum Exploration Qingyang GanSu 745113);Distribution of Sedimentary Facies Belts and Sandstone Bodies of Permo Carboniferous in the Central Part of Ordos Basin[J];ACTA SEDIMENTOLOGICA SINICA;1999-03
6 ZHAO Hong-ge LIU Chi-yang (Department of Geology of Northwest University,Xi’an 710069 );Approaches and Prospects of Provenance Analysis[J];Acta Sedimentologica Sinica;2003-03
7 WANG Yong-dong 1 JIANG De-xin 2 XIE Xiao-ping 3,4 1(Nanjing Institute of Geology and Paleontology, Chinese Academy of Sciences, Na njing 210008) 2(Lanzhou Institute of Geology, Chinese Academy of Sciences, Lanzhou 730000) 3(State Key Laboratory of Estuarine and Coastal Research,East China Normal Unive rsity,Shanghai 200062) 4(Department of Geography,Qufu Normal University,Qufu Shandong 273165);Late Triassic Palynoflora and Its Environmental Significance of Tuweihe, Shaanxi[J];Acta Sedimentologica Sinica;2003-03
8 YAN Ji hua 1 CHEN Shi yue 1 SONG Guo qi 2 JIANG Zai xing 1 QIU Gui qiang 2 1 (Faculty of Geo Resources and Information, University of Petroleum, Dongying, Shandong 257061) 2 (Geological Scientific Research Institute, Shengli Petroleum Administration, Dongying, Shandong257015);Preliminary Study on the Formation of Fluxoturbidite in Front of Delta[J];Acta Sedimentologica Sinica;2004-04
9 Li Wenhou 1 Lin Jinyan 1 Yuan Mingsheng 2 and Wang Wuhe 2 1\ (Depatment of Geology, Northwest University, Xi′an\ 710069) 2\ (Research Group of Petroleum Exploration and Development Headquarters in Turpan Hami, Hami\ 73900);Two Types of Coarse Claslic Delta in Turpan Hami Basin[J];ACTA SEDIMENTOLOGICA SINICA;1996-03
10 Liu Shaofeng Ke Airong Wu Liyun and Huang Siji (China University of Geosciences, Wuhan 430074);Sediment Provenance Analysis and Its Tectonic Significance in the Foreland Basin of the Ordos Southwestern Margin[J];ACTA SEDIMENTOLOGICA SINICA;1997-01
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