Orogenic Garnet Peridotite-Tools to Reconstruct Paleo-geodynamic Settings of Continental Collision Zones

作     者：ZHANG Cong Van ROERMUND Herman 

作者机构：Institute of Geology Chinese Academy of Geosciences Beijing 100037 China Dept. of Earth Sciences Structural Geology and Tectonics Utrecht University Utrecht The Netherlands 

出 版 物：《Acta Geologica Sinica(English Edition)》 (地质学报（英文版）)

年 卷 期：2015年第89卷第A2期

页      面：110-110页

核心收录：

学科分类：070904[理学-构造地质学] 0709[理学-地质学] 070901[理学-矿物学、岩石学、矿床学] 07[理学] 

主　　题：RESEARCH Orogenic belts Garnet High pressure geosciences Olivine Peridotite Metamorphic rocks 

摘      要：Orogenic garnet peridotites （metamorphic rocks containing the characteristic HP garnet-olivine mineral assemblage） exposed in ancient orogenic belts may contain quantitative data regarding formation of subcontinental/ subcratonic lithosphere, evolution of a lithospheric mantle wedge, incorporation of garnet peridotite into subducted continental crust, subsequent （ultra-）high pressure metamorphism during ongoing continental subduction and final exhumation back to subcrustal levels.