| 玄武岩中石英绿帘石型层内错动带成因初探 |
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| 引用本文： | 周志东,苏生瑞.玄武岩中石英绿帘石型层内错动带成因初探[J].四川水力发电,1999,18(1):75-77. |
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| 作者姓名： | 周志东 苏生瑞 |
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| 作者单位： | 成都理工学院,成都,610059 |
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| 摘 要： | 在我国西南地区许多水电站坝区岩体中，缓倾角的层内错动带发育相当普遍，它们对岩体的局部稳定性起控制作用。在某玄武岩坝址区，发育有几种类型的层内错动带，本文对其中的石英绿帘石型层内错动带的成因进行了初步探讨。
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| 关 键 词： | 石英绿帘石 层内错动带 成因 |
| 修稿时间： | :1997-12-1 |
Genetic Analysis on Intraformational Faulted Zones of Quartz-acanthconite in Basult |
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| Zhou Zhidong,Su Shengrui.Genetic Analysis on Intraformational Faulted Zones of Quartz-acanthconite in Basult[J].Sichuan Water Power,1999,18(1):75-77. |
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| Authors: | Zhou Zhidong Su Shengrui |
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| Abstract: | In rock mass in damsite areas of numerous hydropower stations at southwest region in China,intraformational faulted zones with low dip angle are generally developed,which play a decisive role in stability of rock mass.At a basult damsite area,several types of intraformational faulted zones are developed.The genetic analysis on intraformational faulted zones of quartz acanthconite are discussed preliminarily. |
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| Keywords: | quartz acanthconite intrafomational faulted zones genesis |
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