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Article Navigation >  Acta Sedimentologica Sinica  > 2005  >  23(2): 240-247

WEI Ping-sheng, LI Tian-shun, LI An-chun, WANG Jian-gong. Carbon iferous Sedimentary Evolution and Reservoir Estimation in Bayanhot Basin[J]. Acta Sedimentologica Sinica, 2005, 23(2): 240-247.
Citation: WEI Ping-sheng, LI Tian-shun, LI An-chun, WANG Jian-gong. Carbon iferous Sedimentary Evolution and Reservoir Estimation in Bayanhot Basin[J]. Acta Sedimentologica Sinica, 2005, 23(2): 240-247.
shu

Carbon iferous Sedimentary Evolution and Reservoir Estimation in Bayanhot Basin

  • 1.

    Institute of Oceanology, Chinese Academy of Sciences, Qingdao Shandong 266071;

  • 2.

    Graduate School of Chinese Academy of Sciences, Beijing 100039;

  • 3.

    Northwest Branch of PetroChina,Lanzhou 730020;

  • 4.

    China University of Geoscience, Beijing 100083

  • Received Date: 2004-07-07
  • Rev Recd Date: 2004-12-08
  • Publish Date: 2005-06-10
  • This paper researched sedimentary styles and characteristics and discussed about Carboniferous sedimentary evolution of different stages, and, furthermore, analyzed characteristics and distribution of carboniferous clastic reservoir, and main controlling elements of geophysical attribution in order to carry out integrative estimation of reservoir in Bayanhot basin. Bayanhot basin has three depositional systems including lagoon-tidal flat, delta-fan delta and offshore shallow sea. Sedimentary evolution underwent three stages included in the evaporation sea bay of the earlier stage, shallow sea basin of the middle stage, extensive sea of the continentalmargin. Sand bar sub-facies of la- goon, front delta, sheet sandstone of offshore sea are the best sedimentary facies belts for the oil & gas accumulation
  • [1] 1 西安地质学院,玉门石油管理局开发研究院. 甘肃河西走廊东部地区石炭纪和二叠纪地层以及沉积相和生储条件研究[M].西安:西北大学出版社,1989.

    2 刘绍平. 巴彦浩特盆地的构造类型[J].西南石油学院报,2003,(03):24-27.

    3 王增吉. 中国地层(8)-中国的石炭系[M].北京:地质出版社,1990.

    4 林畅松. 贺兰拗拉槽盆地充填演化分析[M].北京:地质出版社,1995.

    5 曹代勇. 河西走廊-巴彦浩特盆地石炭系含油气远景[J].西北地质,2003,(01):63-69.

    6 刘宝珺. 沉积岩石学[M].北京:地质出版社,1980.
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Publishing history
  • Received:  2004-07-07
  • Revised:  2004-12-08
  • Published:  2005-06-10

Carbon iferous Sedimentary Evolution and Reservoir Estimation in Bayanhot Basin

  • 1. Institute of Oceanology, Chinese Academy of Sciences, Qingdao Shandong 266071;
  • 2. Graduate School of Chinese Academy of Sciences, Beijing 100039;
  • 3. Northwest Branch of PetroChina,Lanzhou 730020;
  • 4. China University of Geoscience, Beijing 100083
  • Received Date: 2004-07-07
  • Rev Recd Date: 2004-12-08
  • Publish Date: 2005-06-10

Abstract: This paper researched sedimentary styles and characteristics and discussed about Carboniferous sedimentary evolution of different stages, and, furthermore, analyzed characteristics and distribution of carboniferous clastic reservoir, and main controlling elements of geophysical attribution in order to carry out integrative estimation of reservoir in Bayanhot basin. Bayanhot basin has three depositional systems including lagoon-tidal flat, delta-fan delta and offshore shallow sea. Sedimentary evolution underwent three stages included in the evaporation sea bay of the earlier stage, shallow sea basin of the middle stage, extensive sea of the continentalmargin. Sand bar sub-facies of la- goon, front delta, sheet sandstone of offshore sea are the best sedimentary facies belts for the oil & gas accumulation

WEI Ping-sheng, LI Tian-shun, LI An-chun, WANG Jian-gong. Carbon iferous Sedimentary Evolution and Reservoir Estimation in Bayanhot Basin[J]. Acta Sedimentologica Sinica, 2005, 23(2): 240-247.
Citation: WEI Ping-sheng, LI Tian-shun, LI An-chun, WANG Jian-gong. Carbon iferous Sedimentary Evolution and Reservoir Estimation in Bayanhot Basin[J]. Acta Sedimentologica Sinica, 2005, 23(2): 240-247.
shu

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