鄂西清江中游半峡背斜变形结构及其工程意义

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鄂西清江中游半峡背斜变形结构及其工程意义

吴树仁, 徐瑞春, 梅应堂, 简文星, 刘志忠

文章导航 > 地质力学学报 > 1996 > 2(1): 55-61

吴树仁, 徐瑞春, 梅应堂, 等, 1996. 鄂西清江中游半峡背斜变形结构及其工程意义. 地质力学学报, 2 (1): 55-61.

引用本文:

吴树仁, 徐瑞春, 梅应堂, 等, 1996. 鄂西清江中游半峡背斜变形结构及其工程意义. 地质力学学报, 2 (1): 55-61.

Wu Shuren, Xu Ruichun, Mei Yingtang, et al., 1996. THE DEFORMATIONAL TEXTURE OF THE BANXIA ANTICLNE AND ITS BEARING ON ENGINEERING GEOLOGY OF MIDDLE QINGJIANG RIVER IN WESTERN HUBEI. Journal of Geomechanics, 2 (1): 55-61.

Citation:

Wu Shuren, Xu Ruichun, Mei Yingtang, et al., 1996. THE DEFORMATIONAL TEXTURE OF THE BANXIA ANTICLNE AND ITS BEARING ON ENGINEERING GEOLOGY OF MIDDLE QINGJIANG RIVER IN WESTERN HUBEI. Journal of Geomechanics, 2 (1): 55-61.

吴树仁, 徐瑞春, 梅应堂, 等, 1996. 鄂西清江中游半峡背斜变形结构及其工程意义. 地质力学学报, 2 (1): 55-61.

引用本文:

吴树仁, 徐瑞春, 梅应堂, 等, 1996. 鄂西清江中游半峡背斜变形结构及其工程意义. 地质力学学报, 2 (1): 55-61.

Wu Shuren, Xu Ruichun, Mei Yingtang, et al., 1996. THE DEFORMATIONAL TEXTURE OF THE BANXIA ANTICLNE AND ITS BEARING ON ENGINEERING GEOLOGY OF MIDDLE QINGJIANG RIVER IN WESTERN HUBEI. Journal of Geomechanics, 2 (1): 55-61.

Citation:

Wu Shuren, Xu Ruichun, Mei Yingtang, et al., 1996. THE DEFORMATIONAL TEXTURE OF THE BANXIA ANTICLNE AND ITS BEARING ON ENGINEERING GEOLOGY OF MIDDLE QINGJIANG RIVER IN WESTERN HUBEI. Journal of Geomechanics, 2 (1): 55-61.

鄂西清江中游半峡背斜变形结构及其工程意义

1. 中国地质科学院地质力学研究所, 北京;
2. 长江水利委员会三峡勘测研究院, 宜昌;
3. 中国地质大学, 武汉

基金项目:

本文为国家自然科学基金资助项目和长江水利委员会资助项目的部分成果

作者简介:
吴树仁,男,40岁,副教授,博士后。主要从事地质力学、区域工程地质学和构造地质学等方面的研究。通讯地址:北京海淀区民族学院南路11号地质力学研究所。邮政编码:100081。

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出版历程
- 刊出日期:

THE DEFORMATIONAL TEXTURE OF THE BANXIA ANTICLNE AND ITS BEARING ON ENGINEERING GEOLOGY OF MIDDLE QINGJIANG RIVER IN WESTERN HUBEI

1. Institute of Geomechanics, CAGS;
2. Survey Institute of Three Gorges, the Yangtze River Water Conservancy Commision, Yichang;
3. China University of Geosciences, Wuhan

摘要: 本文在概要介绍湖北西部清江中游大型水利枢纽水布垭、半峡两比选坝址场区地质背景的基础上,从几何要素、层间褶皱、轴面劈理和派生断层等方面解析半峡背斜的变形结构特征,进而探讨半峡背斜形成发展过程及其对两坝址工程地质条件的影响。为两坝址工程地质条件对比分析开拓新思路。
- 清江中游 /
- 半峡背斜 /
- 变形结构 /
- 工程意义
Abstract: After a brief description of the geological settings of the two dam sites located re-spectively in Shuibuya and Banxia in the middle reaches of the Qingjiang river of westen Hubei province'an analysis of the deformational textures of the Banxia anticline was made in terms of its characteristic geometry, intraformational fold, axial plane cleavage and sec-ondary fault.The texture was formed and developed in the major phase of Yanshanian move-ment.The major engineering geological conditions of these two dam sites sitting on opposite limbs of the anticline are controlled by its deformational texture.
- The middle reaches of Qingjiang river /
- Banxia anticline /
- Deformational texture /
- Engineering significance

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文章访问数: 138
HTML全文浏览量: 37
PDF下载量: 21
被引次数: 0

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