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DOI10.1126/science.255.5052.1663
Raising tibet
Harrison T.M.; Copeland P.; Kidd W.S.F.; Yin A.
发表日期1992
ISSN0036-8075
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
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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).
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