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碳酸盐成岩环境的标志

THE CARBONATE DIAGENESIS AND SEDIMENTARY DEPOSITS

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【作者】 郭一华强子同

【Author】 Qiang Zitong, Gou yihua (Southwest China College of petroleum)

【机构】 西南石油学院西南石油学院

【摘要】 <正> 在碳酸盐沉积物的成岩过程中,每一种成岩作用在不同的成岩环境中的表现形式和特征,无不留下该成岩环境的“烙印”,这种“烙印”就是成岩环境的标志。据此我们能够分析、判断和恢复碳酸盐岩的成岩环境。

【Abstract】 The carbonate diagenesis and diagenetic environmentare important in both theory and practice. The first part of this paper is devoted to the explantion of the "diagenetic frap ". Diagenesis controls the distrlution of oil and gas. sometimes a new trapis formed by thiess diagenesis. Hence comes the term "diagenetic trap" In the second part, the formation of sedmentary deposits is discussed. There are dissenting views when the geologists talk about sedimentary deposits if they are formed by diagenesis. The authors of this paper argue that some of sedimentary deposare formed by sedimentation, while others are replaced in the diagenesis. It followies that certain sedimentary deposits must be formed by diagenesis.

  • 【文献出处】 矿物岩石 ,Journal of Mineralogy and Petrology , 编辑部邮箱 ,1983年01期
  • 【被引频次】9
  • 【下载频次】321
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