Xinjiang Petroleum Geology ›› 2004, Vol. 25 ›› Issue (1): 33-36.

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Establishment of Jurassic Sequence Framework in Turpan-Hami Basin

QIN Chang-wen1, LI Hong-wei2, JIANG Bing3   

  1. 1. Research Center of Basin and Reservoir, University of Petroleum 102249, China;
    2. China University of Geosciences,Beijing 100083, China;
    3. Tu-Ha Oilfield Company, PetroChina, Hami, Xinjiang 839000, China
  • Received:2003-05-21 Online:2004-02-01 Published:2020-08-06

Abstract: Turpan-Hami basin is a continental petroliferous basin in which Jurassic is its major prospected stratum. By using theory and methodof high-resolution sequence stratigraphy, comprehensive studies of the outcrop section, drilling and seismic data are made, and the Jurassic isdivided into seven sequences (SQ,-SQ-). SQ, corresponds to Badaowan formation and Sangonghe formation; SQ, to the first, second and thirdmembers of X ishanyao formation;SQ3 to the fourth member of Xishanyao and the first member of Sanjianfang formation; SQ4 to the second andthird members of Sanjianfang; SQs, SQ6 and SQ- to Qiketai, Qigu and Kalazha formations, respectively. The coal measures source rocks are mostdistributed in the upper part of SQ1 and SQ-base-level rising hemicyclothem; the reservoir mainly in SQ,-SQ5 rising hemicyclothems. The SQ3,SQ4 and SQ5 base-level falling lenicylothemas well as SQ6 and SQ6 and SQ7 are the majorizons sf regional cap rocks in this basin.

Key words: Turpan-Hami basin, Jrassic, sequence, boundary, sequence sratigaphy

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