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TAN Xian-feng, TIAN Jing-chun, BAI Jian-ping, WANG Yan-bi, QIU Gui-qiang, ZHANG Shou-peng. Depositional response and filling process of the steep slope rift belt in the terrestrial fault basin: a case study of Paleogene in Dongying terrestrial fault basin[J]. GEOLOGY IN CHINA, 2010, 37(2): 298-310.
Citation: TAN Xian-feng, TIAN Jing-chun, BAI Jian-ping, WANG Yan-bi, QIU Gui-qiang, ZHANG Shou-peng. Depositional response and filling process of the steep slope rift belt in the terrestrial fault basin: a case study of Paleogene in Dongying terrestrial fault basin[J]. GEOLOGY IN CHINA, 2010, 37(2): 298-310.
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Depositional response and filling process of the steep slope rift belt in the terrestrial fault basin: a case study of Paleogene in Dongying terrestrial fault basin

  • 1.

    Chongqing University of Science and Technology, Chongqing 401331, China

  • 2.

    State Key Laboratory for Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, Sichuan, China

  • 3.

    Geological Institute of Shengli Oilfield, Dongying 257015, Shandong, China

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  • Abstract：Syndepositional rift obviously controls the deposition-filling process of the steep slope rift belt in the terrestrial fault basin. Two key rifts, i.e., Chenlan and Shengbei, are developed along the steep slope rift belt in Dongying terrestrial fault basin. The Chenlan rift controls the basin evolution, whereas the Shengbei rift controls the deposition. Clastic components in the steep slope rift belt chiefly came from Chenjiazhuang bulge, Binxian bulge and Qingtuozi bulge. Controlled by the tectonic setting and provenance, alluvial fan, fan-delta, nearshore subaqueous fan, delta and fluxoturbidite-fan were filled in the steep slope rift belt. There exists a typical temporal and spatial evolution in order of alluvial fan→nearshore subaqueous fan→fan-delta→fluxoturbidite-fan→lake. Having good physical properties and strong tectonic activities and being close to oil sources, the steep slope rift belt constitutes a favorable oil and gas accumulation place.
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