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ZHU Yu-shuang, LIU Yi-qun, ZHOU Ding-wu. Origin of Dolostone in Lucaogo Formaion of Middle Permian in Santanghu Basin[J]. Northwestern Geology, 2009, 42(2): 95-99.
Citation: ZHU Yu-shuang, LIU Yi-qun, ZHOU Ding-wu. Origin of Dolostone in Lucaogo Formaion of Middle Permian in Santanghu Basin[J]. Northwestern Geology, 2009, 42(2): 95-99.
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Origin of Dolostone in Lucaogo Formaion of Middle Permian in Santanghu Basin

  • State Key Labortory of Continantal Dynamics, Department of Geology, Northwest University, Xi'an, Shaanxi 710069, China

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  • Received Date: September 22, 2008
  • Revised Date: March 09, 2009
  • Published Date: June 04, 2009
    Graphical Abstract
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  • Carbonate rock of Lucaogou Formation in Middle Permian is a major reservoir rock in Santanhu Basin and dolost one accounts for more than 50% in composition of the carbonate rock.There are two types of dolo stone,one is the bedded dolostone and the other is the patch dolomite.In the bedded dolostone,the mineral dolomite has a good idiomorphism;on the contrary,in the patch dolostone,the idiomorphism of dolomite is not good.The patch dolostone is composed of ankerite with crassitude crystal replacing calcite.
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