Multiple Successions of Soliation Development in Shallow Versus Deep Orogenic Regimes and Their Relationship to Regional Folding

作     者：Hui Cao State Key Laboratory of Geological Processes and Mineral Resources Institute of Land Resources and High Techniques,China University of Geosciences(Beijing),Beijing 100083,China. 

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

年 卷 期：2009年第16卷第S1期

页      面：89-90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：orogenesis axial planes of folds porphyroblasts foliation intersection/inflection axes(FIAs) 

摘      要：With the realization that rocks with a schistosity parallel to bedding(S0 parallel S1)have undergone lengthy histories of deformation that predate the obvious first deformation(*** et al.,2003; Sayab,2006;Yeh,2007)came recognition that large scale regional folds can form early during this process and be preserved throughout orogenesis(e.g.,Ham & Bell,2004;Bell & Newman,2006).This history is lost within the matrix because of reactivational shear