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恩洪矿区古构造应力场特征及演化

he region of ancient tectonic stress field feature and evolution of Enhong mine

中文摘要英文摘要

在区域构造研究的基础上,通过对研究区节理发育特征的分析,表明恩洪矿区节理优势方位为NE向,其发育NNW-SSE两组。通过对相关共轭节理系统的统计分析,显示在区域构造应力场的控制下,可将研究区构造应力场分为以下三个主要期次:印支期近S-N向挤压应力;燕山晚期-喜马拉雅早期NNW-SSE向挤压(或拉张);喜马拉雅晚期NNW-SEE向挤压。

On the basis of the regional tectonic background research in the study area, through the analysis of characteristics of the joints growth shows that the orientation preferred of joints is NE, second orientation are NNW and NWW. Based on the statistical analysis of conjugate joints system, under the control of the regional tectonic stress, the tectonic stress field in late into coal period of study area can be divided into three main period: In Indochina period the principal stress direction is S - N, In late Yanshanian - early Himalayan period the principal stress direction is NNW - SSE, In late Himalayan period the principal stress direction is NWW - SEE.

帅伟、王继尧

矿山地质、矿山测量地质学

构造应力场恩洪矿区构造演化

tectonic stress fieldEnhong minetectonic evolution

帅伟,王继尧.恩洪矿区古构造应力场特征及演化[EB/OL].(2014-03-07)[2025-07-16].http://www.paper.edu.cn/releasepaper/content/201403-254.点此复制

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