| 资阳地区震旦系灯影组白云岩成因研究 |
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| 引用本文： | 王士峰,向芳.资阳地区震旦系灯影组白云岩成因研究[J].沉积与特提斯地质,1999,19(3):21-29. |
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| 作者姓名： | 王士峰 向芳 |
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| 作者单位： | 成都理工学院,沉积研究所,四川,成都,610059 |
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| 摘 要： | 本文通过实际资料将资阳地区震旦系灯影组划分为四种主要岩石类型及三种主要沉积相。依据最新的白云岩成因理论，结合先进的室内测试手段，对这几类白云岩进行成因分析，证明资阳地区灯影组白云岩具原生和重结晶两种成因类型。
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| 关 键 词： | 资阳 灯影组 白云岩 原生 重结晶 |
| 收稿时间： | 1998/11/20 0:00:00 |
| 修稿时间： | 1998-11-20 |
The origin of the dolostones from the Sinian Dengying Formation in the Ziyang district,Sichuan |
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| WANG Shi-feng,XIANG Fang.The origin of the dolostones from the Sinian Dengying Formation in the Ziyang district,Sichuan[J].Sedimentary Geology and Tethyan Geology,1999,19(3):21-29. |
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| Authors: | WANG Shi-feng XIANG Fang |
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| Institution: | Chengdu University of Technology, Chengdu 610059, China |
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| Abstract: | The Sinian Dengying Formation in the Ziyang district, Sichuan contains a succession of dolostones with abundant blue green algae. Four rock types have been distinguished. They are algae binding dolostone, algal dolostone, dolomicrite and dolosiltite, which are arranged into subtidal subfacies, intertidal subfacies and supratidal subfacies, respectively. The additional types include dark grey and bluish grey mudstones and muddy dolostones. According to latest theory and approach to the origin of dolostones, the dolostones from the study area are interpreted to be partly primary in origin or originated from recrystallization. |
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| Keywords: | Ziyang Dengying Formation dolostone primary recrystallization |
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