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DOI | 10.1126/science.255.5052.1663 |
Raising tibet | |
Harrison T.M.; Copeland P.; Kidd W.S.F.; Yin A. | |
发表日期 | 1992 |
ISSN | 0036-8075 |
起始页码 | 1663 |
结束页码 | 1670 |
卷号 | 255期号:5052 |
英文摘要 | Thermochronologic, sedimentologic, oceanographic, and paleoclimatic studies suggest that rapid uplift and unroofing of southern Tibet began about 20 million years ago and that the present elevation of much of the Tibetan plateau was attained by about 8 million years ago. Hypotheses advanced to explain the tectonic evolution of the India-Asia collision, which began about 40 to 50 million years ago, predict the timing and rates of crustal thickening of the southern margin of Asia. However, these models do not predict the prominently enhanced early Miocene denudation and uplift that are manifested in a variety of geological records. A model involving continental extrusion, development of a crustal-scale thrust ramp of the Main Central Thrust beneath the Gangdese belt, and lithospheric delamination provides a history consistent with these observations. |
英文关键词 | collision; lithospheric delamination; Miocene; plate tectonic model; tectonic evolution; thrust ramp; unroofing; uplift; China, Tibet |
语种 | 英语 |
来源期刊 | Science |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/243954 |
作者单位 | Institute of Geophysics and Planetary Physics, Department of Earth and Space Sciences, University of California, Los Angeles, Los Angeles, CA 90024, United States; Department of Geosciences, University of Houston, Houston, TX 77204, United States; Department of Geological Sciences, State University of New York at Albany, Albany, NY 12222, United States |
推荐引用方式 GB/T 7714 | Harrison T.M.,Copeland P.,Kidd W.S.F.,et al. Raising tibet[J],1992,255(5052). |
APA | Harrison T.M.,Copeland P.,Kidd W.S.F.,&Yin A..(1992).Raising tibet.Science,255(5052). |
MLA | Harrison T.M.,et al."Raising tibet".Science 255.5052(1992). |
条目包含的文件 | 条目无相关文件。 |
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