Lithologic Reservoirs ›› 2008, Vol. 20 ›› Issue (2): 6-15.doi: 10.3969/j.issn.1673-8926.2008.02.002

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Resear ch status of dolomite genesis and its problems in Sichuan Basin

LIU Shugen1, HUANG Wenming1, ZHANG Changjun1, ZHAO Xiafei1, DAI Sulan2,ZHANG Zhijing1, QIN Chuan1   

  1. 1. State Key Laboratory ofOil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China; 2. Sichuan Institute of Product Quality Supervision and Inspection, Chengdu 610031, China
  • Online:2008-06-15 Published:2008-06-15

Abstract:

The formations from the Upper Sinian toMiddle Triassic in Sichuan Basin are marine deposits and mainly composed of carbonate rocks. Through 50 years petroleum exploration, fifteen carbonate gas-bearing beds have been found in the basin. Among them, carbonate rocks of Upper Sinian and Cambrian have been completely dolomitized, and the others also have dolomitization more or less. There are various explanations for the genetic model of dolomite in marine carbonate reservoir in Sichuan Basin, mainly including: protogene, penecontemporaneous, reflux, meteoric-seawater mixing water, burial, hydrothermal fluid, leaching of basalt and biogenesis. Dolomite reservoir is regarded as one of the most important carbonate reservoir, and the dolomitization is the prerequisite for the development of high-quality carbonate reservoirs in Sichuan Basin. The burial dolomitization and meteoric-seawater mixing dolomitization of marine carbonate rocks have been widely queried, and there are two taphrogenesis events and related extensive fluid activities in marine carbonate rocks in Sichaun Basin, so hydrothermal dolomitization could be more widespread than previously thought in Sichuan Basin.

Key words: seismite, event deposit, seismite vertical sequence, identification mark, Paleogene, Yangxin Subsag

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