Orogen-parallel extension in Himalaya: Is it the indicator of collapse or the product in process of compressive uplift?
文献类型:期刊论文
作者 | Zhang, JJ; Ding, L; Zhong, DL; Zhou, Y |
刊名 | CHINESE SCIENCE BULLETIN |
出版日期 | 2000 |
卷号 | 45期号:2页码:114-120 |
ISSN号 | 1001-6538 |
关键词 | Himalayan orogenic belt syn-shortening extension uplift |
文献子类 | Article |
英文摘要 | Extensional structures developed extensively in Himalaya with their strikes perpendicular to that of the orogenic belt. The studies of such structures in Qusum, Burang, Lhozhag, Nyalam and Yadong show that they represent an orogen-parallel extension. The basins produced by the extension experienced orogen-perpendicular compression during their formation. The ages of the extension rang from 16 to 13 Ma and coincide with the intensive compressive stage in Southeastern Asia, Therefore, the extension is syn-shortening and the dominate tectonic movement in Himalaya was compression and uplift during the extension. The extension was the partition of compressive deformation rather than the indicator for the collapse and falling of the Tibetan Plateau. |
WOS关键词 | TIBETAN PLATEAU ; SOUTHERN TIBET ; DEFORMATION ; TECTONICS |
WOS研究方向 | Science & Technology - Other Topics |
语种 | 英语 |
出版者 | SCIENCE PRESS |
WOS记录号 | WOS:000085980400004 |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/76107] |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Zhang, JJ |
作者单位 | Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China |
推荐引用方式 GB/T 7714 | Zhang, JJ,Ding, L,Zhong, DL,et al. Orogen-parallel extension in Himalaya: Is it the indicator of collapse or the product in process of compressive uplift?[J]. CHINESE SCIENCE BULLETIN,2000,45(2):114-120. |
APA | Zhang, JJ,Ding, L,Zhong, DL,&Zhou, Y.(2000).Orogen-parallel extension in Himalaya: Is it the indicator of collapse or the product in process of compressive uplift?.CHINESE SCIENCE BULLETIN,45(2),114-120. |
MLA | Zhang, JJ,et al."Orogen-parallel extension in Himalaya: Is it the indicator of collapse or the product in process of compressive uplift?".CHINESE SCIENCE BULLETIN 45.2(2000):114-120. |
入库方式: OAI收割
来源:地质与地球物理研究所
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