LITHOLOGIC RESERVOIRS ›› 2015, Vol. 27 ›› Issue (1): 66-73.doi: 10.3969/j.issn.1673-8926.2015.01.010

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Sedimentary microfacies analysis of the Middle Triassic Leikoupo Formation-Tianjingshan Formation boundary in Hanzeng area, Jiangyou

LIU Chiheng 1,2,3, HU Zuowei 1,2, LI Yun 1,2, LUO Wen 1,2   

  1.  1. Institute of Sedimentary Geology , Chengdu University of Technology , Chengdu 610059 , China ; 2. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation , Chengdu University of Technology , Chengdu 610059 , China ; 3. Key Laboratory of Tectonic Controls on Mineralization and Hydrocarbon Accumulation , Ministry of Land and Resources , Chengdu University of Technology , Chengdu 610059 , China
  • Online:2015-02-03 Published:2015-02-03

Abstract:

 The distribution range of Middle Triassic Tianjingshan Formation is limited to the northwest Sichuan Basin, affected by the Indosinian movement. The in-depth study of sedimentary transformation from Leikoupou Formation to Tianjingshan Formation of Middle Triassic is of great significant to understand the sedimentary environment evolution. By measuring the field profile of the Middle Triassic Leikoupo Formation-Tianjingshan Formation boundary in Hanzeng area and observing microfacies characteristics indoor, we identified five types of microfacies according to fossil assemblages, granular characteristics, filler types and architecture features of carbonate rocks, and recognized four sedimentary facies belts, including platform-margin sand shoal, open platform, restricted platform and evaporate platform. Based on the longitudinal change characteristics of sedimentary facies belts, it is concluded that sea level in Hanzeng area presents overall rise for a long period, and salt sea desalts gradually from Anisian Age to Ladinian Age in Middle Triassic.

Key words: sedimentary sequence, stratigraphic unconformity trap, Jurassic, Sarybulak, South Turgai Basin

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