The source rocks of Ordovician carbonate rocks in the Ordos Basin are mostly Preserved in darkgrey micrite transgtessive system tracts and early-sarge high water-level system tracts.

 
  • 應用層序地層學(xué)基本原理對奧陶系碳酸鹽巖含油氣性的研究表明:一方面構成奧陶系層序格架的不同單元,具有各異的油氣地質(zhì)意義;
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