| 青藏高原的隆升：青藏高原的岩石圈结构和构造地貌 |
| |
| 引用本文： | 崔军文,李朋武,等.青藏高原的隆升：青藏高原的岩石圈结构和构造地貌[J].地质论评,2001,47(2):157-163. |
| |
| 作者姓名： | 崔军文 李朋武 |
| |
| 作者单位： | 中国地质科学院地质研究所,北京,100037 |
| |
| 摘 要： | 笔者回顾青藏高原隆升研究的历史，剖析各种隆升动力学模式，依据着青藏高原岩石圈组成的构的强烈不均一性和、三分性”，“对称性”构造地貌格局，提出了青藏高原隆升是印度地块和塔里木一可拉善地块双向不均一俯冲和青藏腹地深层热隆扩展联合作用的结果，俯冲是高原隆升的重要机制，而热隆扩展是高原隆升的直接原因。
|
| 关 键 词： | 隆升 俯冲 岩石圈结构 构造地貌 青藏高原 热隆扩展 |
Uplift of the Qinghai-Tibet Plateau: Tectonic Geomorphology and Lithospheric Structure of the Qinghai-Tibet Plateau |
| |
| CUI Junwen,LI Pengwu,LI LiInstitute of Geology,Chinese Academy of Geological Sciences,Beijing.Uplift of the Qinghai-Tibet Plateau: Tectonic Geomorphology and Lithospheric Structure of the Qinghai-Tibet Plateau[J].Geological Review,2001,47(2):157-163. |
| |
| Authors: | CUI Junwen LI Pengwu LI LiInstitute of Geology Chinese Academy of Geological Sciences Beijing |
| |
| Abstract: | Through a review of the research history of the Qinghai-Tibet Plateau uplift and analysis of various dynamic models of the uplift, a dynamic model of the Qinghai-Tibet Plateau uplift, deep thermal uplift spreading, is suggested on the basis of the intensive inhomogeneity of the lithosphere fabrics and structural geomorphologic pattern of tridivision and symmetry. The uplift of the Qinghai-Tibet Plateau is a synthetic result of the bidirectional inhomogeneous subduction of the India block and Tarim-Alxa block and deep thermal-uplift spreading of the Qinghai-Tibet hinterland. Subduction is an important mechanism of the uplift, and deep thermal-uplift spreading is the direct cause. |
| |
| Keywords: | uplift subduction thermal-uplift spreading lithospheric structure structural geomorphology |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
| 点击此处可从《地质论评》浏览原始摘要信息 |
|
点击此处可从《地质论评》下载全文 |
