Eocene Crustal Thickening and Uplifting of the Tibetan Plateau:Evidence from Adakitic Volcanic Rocks

作     者：Derek A.Wyman 

作者机构：School of GeosciencesDivision of Geology and GeophysicsThe University of Sydney 

出 版 物：《地学前缘》 (Earth Science Frontiers)

年 卷 期：2009年第16卷第S1期

页      面：274-274页

核心收录：

学科分类：070904[理学-构造地质学] 0709[理学-地质学] 07[理学] 

主　　题：adakites high-Mg andesites subduction uplift Eocene icehouse Tibet 

摘      要：Changes in oceanic O-Sr-C isotopic compositions, global cooling and Asian continental aridification beginning in the Middle-Late Eocene(47-34 Ma) are considered to have been caused by the uplift of the Tibetan *** specific timing and uplift mechanism,however,have long been subjects of *** investigated the Duogecuoren lavas of the central-western Qiangtang block,which form the largest outcrops among Cenozoic lavas in north-