| 滇西北金沙江结合带吉义独斜向走滑韧性剪切带特征 |
| |
| 引用本文： | 江元生,葛孟春,冯庆来. 滇西北金沙江结合带吉义独斜向走滑韧性剪切带特征[J]. 矿物岩石, 2001, 21(4): 31-35 |
| |
| 作者姓名： | 江元生 葛孟春 冯庆来 |
| |
| 作者单位： | 1. 成都理工大学,
2. 中国地质大学地球科学学院, |
| |
| 摘 要： | 滇西北金沙江喧是三江古特提斯构造域中关键地段之一，其内斜向走滑构造最为夺目。本文以1：5万霞若幅、中甸县幅区域地质调成果，从剪切带的物质组成、变形特征、矿物的应变象和运动学特征方面论述了金沙江结合带中最重要的一条斜向走滑剪切带－吉义独斜向走滑韧性剪切带。
|
| 关 键 词： | 斜向走滑 韧性剪切带 金沙江结合带 滇西北吉义独地区 |
| 文章编号： | 1001-6872(2001)04-0031-05 |
FEATURE OF JIYIDU OBLIQUE STRIKE-SLIP DUCTILE SHEAR ZONE IN THE JINSHAJIANG COMBINED BELT, NORTHWEST YUNNAN |
| |
| JIANG Yuan-sheng GE Meng-chun FENG Qing-lai. FEATURE OF JIYIDU OBLIQUE STRIKE-SLIP DUCTILE SHEAR ZONE IN THE JINSHAJIANG COMBINED BELT, NORTHWEST YUNNAN[J]. Journal of Mineralogy and Petrology, 2001, 21(4): 31-35 |
| |
| Authors: | JIANG Yuan-sheng GE Meng-chun FENG Qing-lai |
| |
| Affiliation: | JIANG Yuan-sheng 1 GE Meng-chun 2 FENG Qing-lai 2 |
| |
| Abstract: | There are some oblique strike-slip structures in the Jingshajiang combined zone which is one of the key regions in the Sanjiang Paleotethyan tectonic donmain.Data of 1/50000 geological survey are used to study the material compositions,strain,deformation and kinematic characteristics in the Jiyidu oblique strike-slip ductile shear zone. |
| |
| Keywords: | oblique strike-slip ductile shear zone Jingshajiang combined zone Jiyidu Northwest Yunnan |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
