Xinjiang Petroleum Geology ›› 2009, Vol. 30 ›› Issue (1): 68-72.

Previous Articles     Next Articles

Sedimentary Facies of Triassic in Hong-Che Area in Junggar Basin

WANG Ya-ning1a,1b, ZHANG Shang-feng1b, ZHAO Wei-jun2, LIANG Ze-liang2   

  1. 1. Yangtze University, a.Key Laboratory of Exploration Technologies for Oil and Gas Resources, Ministry of Education; b.College of Geosciences, Jingzhou, Huibei 434023, China;
    2. Institute of Geophysics, Research Institute of Exploration and Development, Xinjiang Oilfield Company, PetroChina, Urumqi, Xinjiang 830013, China
  • Received:2008-04-25 Revised:2008-04-25 Online:2009-02-01 Published:2020-08-21

Abstract: The Triassic in Hongshanzui-Chepaizi area is one of the important petroleum enrichment zones in northwestern margin of Junggar basin. The favorable exploration play assessment is primarily based on the studies of the sedimentary facies of the Triassic. This study identifies multiple sedimentary facies types in this area through core description and analysis, integrated with the log information and seismic data, including alluvial fan, braided river, delta, lake, etc. The braided river deposit in Lower Karamay formation in Hongshanzui area is the favorable facies belt for lithologic reservoir exploration.

Key words: Hong-Che area, Triassic, sedimentary facies, seismic facies, lithologic reservoir

CLC Number: