| 青藏高原北缘昆仑-羊湖地区构造运动及其地质意义 |
| |
| 引用本文： | 戴传固.青藏高原北缘昆仑-羊湖地区构造运动及其地质意义[J].贵州地质,2009,26(2):81-84. |
| |
| 作者姓名： | 戴传固 |
| |
| 作者单位： | 中国地质大学,北京 100083;贵州省地质调查院,贵阳 550005 |
| |
| 基金项目： | 25奥依亚依拉克幅区域地质调查项目成果 |
| |
| 摘 要： | 昆仑-羊湖地区位于青藏高原北缘昆仑山脉中段之南侧，经历了早海西旋回、晚海西旋回和印支旋回洋陆转换阶段的发展及板内造山演化历程，发育早海西运动、晚海西运动、印支运动和燕山运动-喜马拉雅运动，它们分别是洋陆转换和板内造山事件的具体表现。
|
| 关 键 词： | 构造运动 青藏高原 昆仑-羊湖地区 |
Tectonism and Geological Significance in Kunlun- Yanghu Area of North Qinghal- Xizang Plateau |
| |
| Institution: | DAI Chuan - gu( 1. China University of Geosciences, Beijing 100083, China ; 2. Guizhou Academy of Geologic Survey, Guiyang 550005, Guizhou, China) |
| |
| Abstract: | Kunlun -Yanghu area is situated in the north Qinghai -Xizang plateau and the south middle Kunlun Mountain. It experienced the development of early Hercynian cycle, late Hereynian cycle and India Hercynian cycle and intra orogenic plate, the tectonic phenomena of early Hercynian orogeny, late Hercynian orogeny, Indosinian movement and Yanshanian -Ximalaya movement are developed. They are the particular representation of ocean - shore transition and intra orogenic event separately. |
| |
| Keywords: | Tectonism Qinghai - Xizang plateau Kunlun - Yanghu area |
| 本文献已被 维普 万方数据 等数据库收录！ |
|
