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Article Navigation >  Acta Sedimentologica Sinica  > 2001  >  19(3): 386-393

LI Shuang ying, LI Zhong, WANG Zhong cheng, LIU Jian min, WU Chao dong, LI Xiang. The Study of Depositional Model in the Upper Member of Guantao Formation in Gudao Oiifield of the Shengli Petroleum Province[J]. Acta Sedimentologica Sinica, 2001, 19(3): 386-393.
Citation: LI Shuang ying, LI Zhong, WANG Zhong cheng, LIU Jian min, WU Chao dong, LI Xiang. The Study of Depositional Model in the Upper Member of Guantao Formation in Gudao Oiifield of the Shengli Petroleum Province[J]. Acta Sedimentologica Sinica, 2001, 19(3): 386-393.
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The Study of Depositional Model in the Upper Member of Guantao Formation in Gudao Oiifield of the Shengli Petroleum Province

  • 1.

    Department of Natural Resources and Environmental Science Hefei University of Technology Hefei 230009;

  • 2.

    Institute of Geology, Chinese Academy

  • Received Date: 2000-10-08
  • Rev Recd Date: 2000-12-28
  • Publish Date: 2001-09-10
  • On the basis of the characteristics of architectural elements, sandstone grain size analysis, and fluvial styles of the Upper Members of Guantao Formation in Gudao oilfield, and according to stream features of 16 kinds proposed by Miall, we believe that it belongs to fine grain meandering stream. Among architectural elements, floodplain fines (FF), crevasse splay (CS) and lateral accretion macroform (LA) developed extensively, and levee (LV) and crevasse channel (CR) also developed. The channel sinuosity (P) is more than 2.2. The channel is 100～300 meters wide. The channel meander wavelength is 1 000～1 770 meters. The stream may be adjacent to an estuary, and development of sandstone bodies may be subject to fluctuation of sea level.
  • [1] 1.王秉海;钱凯胜利油区地质研究与勘探实践 1992

    2.李兴国;周宪臣孤岛油田两类河流相储集层及其开发效果分析 1982(02)

    3.李阳河道砂储层非均质模型和剩余油分布研究—以胜利油田馆陶组上段油藏为例[学位论文] 2000

    4.Miall A D Architectural-elements analysis:analysis:a new method of facies analysis applied to fluvial deposits 1985

    5.Miall A D 查看详情 1988

    6.Mial1AD The geology of f luvial deposits 1996

    7.Reineck H E;Singh I B Depositional sedimentary environments-with reference to terrigenous clastics 1973

    8.Rust B R A classification of alluvial channel systems 1978

    9.王随继;任明达根据河道形态和沉积物特征的河流新分类[期刊论文]-沉积学报 1999(02)

    10.钱宁关于河流分类及成因问题的讨论[期刊论文]-地理学报 1985(01)

    11.Miall A D 沉积盆地分析原理(中译本,1991) 1984
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Publishing history
  • Received:  2000-10-08
  • Revised:  2000-12-28
  • Published:  2001-09-10

The Study of Depositional Model in the Upper Member of Guantao Formation in Gudao Oiifield of the Shengli Petroleum Province

  • 1. Department of Natural Resources and Environmental Science Hefei University of Technology Hefei 230009;
  • 2. Institute of Geology, Chinese Academy
  • Received Date: 2000-10-08
  • Rev Recd Date: 2000-12-28
  • Publish Date: 2001-09-10

Abstract: On the basis of the characteristics of architectural elements, sandstone grain size analysis, and fluvial styles of the Upper Members of Guantao Formation in Gudao oilfield, and according to stream features of 16 kinds proposed by Miall, we believe that it belongs to fine grain meandering stream. Among architectural elements, floodplain fines (FF), crevasse splay (CS) and lateral accretion macroform (LA) developed extensively, and levee (LV) and crevasse channel (CR) also developed. The channel sinuosity (P) is more than 2.2. The channel is 100～300 meters wide. The channel meander wavelength is 1 000～1 770 meters. The stream may be adjacent to an estuary, and development of sandstone bodies may be subject to fluctuation of sea level.

LI Shuang ying, LI Zhong, WANG Zhong cheng, LIU Jian min, WU Chao dong, LI Xiang. The Study of Depositional Model in the Upper Member of Guantao Formation in Gudao Oiifield of the Shengli Petroleum Province[J]. Acta Sedimentologica Sinica, 2001, 19(3): 386-393.
Citation: LI Shuang ying, LI Zhong, WANG Zhong cheng, LIU Jian min, WU Chao dong, LI Xiang. The Study of Depositional Model in the Upper Member of Guantao Formation in Gudao Oiifield of the Shengli Petroleum Province[J]. Acta Sedimentologica Sinica, 2001, 19(3): 386-393.
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