The geological evolution of Tibet. by Chang Chengfa [and others]
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The geological evolution of Tibet. by Chang Chengfa [and others]

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Published by Royal Society in London .
Written in English

Subjects:

  • Geology - Tibet

Book details:

Edition Notes

ContributionsChengfa, C.
Classifications
LC ClassificationsQE 294 G345 1988
The Physical Object
Pagination413 p.
Number of Pages413
ID Numbers
Open LibraryOL21986475M

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  Buy The Geological Evolution of Tibet (Royal Society Discussion Volumes) on FREE SHIPPING on qualified orders The Geological Evolution of Tibet (Royal Society Discussion Volumes): C. Chengfa, R. M. Shackleton, J. F. Dewey: : Books. This book presents the results of a two month geotraverse of the Tibetan plateau made in through co-operation between the Royal Society and the Academia Sinica. Data from a wide range of geological methods are presented together with a geological map of the area traversed. The final chapter gives the conclusions about the geological evolution. The Geological Evolution of Tibet: Chang Chengfa. Royal Society, - China - Geology - Tibet, Plateau of - pages. 0 Reviews. From inside the book. What people are saying - Write a review. We haven't found any reviews in the usual places. Contents. Buy The geological evolution of Tibet: Report of the Royal Society-Academia Sinica Geotraverse of the Qinghai-Xizang Plateau on FREE SHIPPING on qualified orders.

Buy The Geological Evolution of Tibet by Chengfa, C, Shackleton, R M, Dewey, J F online on at best prices. Fast and free shipping free returns cash on Format: Hardcover. The geological evolution of the Tibetan plateau is best viewed in a context broader than the India-Eurasia collision zone. After collision about 50 million years ago, crust was shortened in. The Geological Evolution of Tibet: Chengfa, C., Shackleton, R. M., Dewey, J. F.: Books - Buy THE GEOLOGICAL EVOLUTION OF TIBET. by Chang & Robert M. Shackleton. Et al. Chengfa (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible : Chang & Robert M. Shackleton. Et al. Chengfa.

  The geological evolution of the Tibetan plateau is best viewed in a context broader than the India-Eurasia collision zone. After collision about 50 million years ago, crust was shortened in western and central Tibet, while large fragments of lithosphere moved from the collision zone toward areas of trench rollback in the western Pacific and Indonesia. Chang Chengfa, The characteristics of evolution of Tethys and collision-orogen in the Qinghai-Xizang Plateau (eds. Xu Guizhong, Chang Chengfa), Continental Lithosphere Tectonic and Resource (in Chinese), Beijing: Ocean Publishing House, , 1– Google Scholar. The Tibetan Plateau, between the Kunlun Shan and the Himalayas, consists of terranes accreted successively to Eurasia. The northernmost, the Songban Ganzi Terrane, was accreted to the Kunlun (Tarim-North China Terrane) along the Kunlun-Qinling Suture during the late Permian.   - Buy The Geological Evolution of Tibet (Royal Society Discussion Volumes) book online at best prices in India on Read The Geological Evolution of Tibet (Royal Society Discussion Volumes) book reviews & author details Format: Hardcover.