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Strata sequence and its mechanisms of the Bachu Formation in the Hudson area,Tarim Basin

Ning Chao-zhong1,2,Xu Huai-min2,Yang Jian-ping3,Sun Hai-hang3,Li Wei-lu2,Su Chen2,Chen Xiao-ran2   

  1. 1.PetroChina Research Institute of Petroleum Exploration & Development,Beijing 100083,China;
    2.College of Geosciences,China University of Petroleum (Beijing),Beijing 102249,China;
    3.PetroChina Tarim Oilfield Company,Korla 841000,China
  • Received:2017-03-01 Revised:2017-06-11 Online:2017-07-10 Published:2017-07-10

Abstract:

The aim of this article is to confirm the strata sequence and the mechanisms of the Bachu Formation of the Hudson area,Tarim Basin and to settle the related debates of the stratigraphic evolution and sedimentary history.Based on the specific analysis on cores,well-logging and regional stratigraphic correlation,it has been proved that the lower mudstone member and bioclastic limestone member exist above the Donghe sandstone member of the Bachu Formation in Hudson.Donghe sandstone member,lower mudstone member,bioclastic limestone member in Hudson were deposited successively during the Early Carboniferous,which constituted the standard sedimentary sequence of the Bachu Formation in the area.This standard sedimentary sequence is identical with those in other areas in the Trim Basin.Because of the later tectonic uplift,differential denudation and mixed deposition,the strata sequence of the Bachu Formation was no longer intact.The Breccia member was generated and five types of strata sequence were formed (from  bottom to top):Ⅰ Donghe sandstone member-lower mudstone member-bioclastic limestone member,Ⅱ Donghe sandstone member-bioclastic limestone member-breccia member,Ⅲ Donghe sandstone member-lower mudstone member,Ⅳ Donghe sandstone member-breccia member and Ⅴ Donghe sandstone member.Each type of strata sequence lies in its own unique area within the Donghe sandstone reservoir area.The recognition of the Bachu Formation in Hudson influences the study of sedimentary environment and sequence,the source of the calcium of the calcareous interlayers and diagenesis in the Donghe sandstone,the application of the seismic data and the petroleum exploration of the area.

Key words: Tarim Basin, Forming mechanisms, Bachu Formation, Sedimentary sequence, Mixed deposition

CLC Number: 

  • TE121.3+4

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