| 白云岩的成因研究现状及最新进展 |
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| 引用本文： | 叶征宇,孙成旺,黄晓东.白云岩的成因研究现状及最新进展[J].四川地质学报,2011(3):266-268. |
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| 作者姓名： | 叶征宇 孙成旺 黄晓东 |
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| 作者单位： | 四川省核工业地质调查院;成都理工大学; |
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| 摘 要： | 白云岩是主要由白云石组成的碳酸盐岩,对其成因的研究一直是沉积岩石学的热点。主要有原生白云石直接沉淀、次生交代和其他成因模式。目前普遍接受的主流成因模式是白云岩由石灰岩经过变化而成的,即石灰岩白云石化。
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| 关 键 词： | 白云岩 成因模式 新进展 |
Present Situation and Advances in Research on Genesis of Dolomitite |
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| YE Zheng-yu SUN Cheng-wang HUANG Xiao-dong.Present Situation and Advances in Research on Genesis of Dolomitite[J].Acta Geologica Sichuan,2011(3):266-268. |
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| Authors: | YE Zheng-yu SUN Cheng-wang HUANG Xiao-dong |
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| Institution: | YE Zheng-yu SUN Cheng-wang HUANG Xiao-dong(1-Sichuan Institute of Geological Survey for Nuclear Industry,Chengdu 610061,2-Chengdu University of Technology,Chengdu 610059) |
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| Abstract: | This paper deals with present situation and advances in research on genesis of dolomitite.Currently,most of sedimentologists believe that dolomitite is formed by dolomitization of limestone. |
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| Keywords: | dolomitite genetic model new progress |
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