| 太白山古冰川地貌与地质构造 |
| |
| 引用本文： | 夏正楷.太白山古冰川地貌与地质构造[J].冰川冻土,1990,12(2):155-160. |
| |
| 作者姓名： | 夏正楷 |
| |
| 作者单位： | 北京大学地理系 |
| |
| 摘 要： |
|
| 关 键 词： | 古冰川 冰川地貌 地质构造 太白山 |
The Ancient Glacial Relief and the Faulting Tectonics in the Taibaishan, Qinling Mts. |
| |
| Xia Zhengkai.The Ancient Glacial Relief and the Faulting Tectonics in the Taibaishan, Qinling Mts.[J].Journal of Glaciology and Geocryology,1990,12(2):155-160. |
| |
| Authors: | Xia Zhengkai |
| |
| Abstract: | The Taibaishan (3767 m), situated in the Mixian, Shaxi Province, is the highest peak of the Qinling Mts, where some glacial lakes and glacial troughs formed during the Quaternary.
The following are their characteristics:
1. The glacial troughs display cross pattern on the horizontal plane.
2. The E-W trending trough exhibits a wide valley in the transverse section, while the N-S trending trough exhibits U-shape.
3. The E-W trending trough is gentle in the longitudinal profile, while the N-S trending trough is stepwise with many scarps crossed the faults.
4. The cirque always developed at the junction of faulting belts.
5. Cirques are small in area and large in depth. Some glacial lakes had specific geometrical form.
It is noted that the glacial relief developed in the Taibaishan area is associated with faulting tectonics. The glacial relief can be mostly explained by,tectonics. The fault fracture zone is favourable to glacier plucking. |
| |
| Keywords: | Taibaishan glacial relief himalayan movement faulting tectonics |
| 本文献已被 CNKI 维普 等数据库收录！ |
|
