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　　处：《地学前缘》2009年第S1期89-90,共2页Earth Science Frontiers

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(e.g.Bell 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

关 键 词：OROGENESIS axial planes of FOLDS PORPHYROBLASTS FOLIATION intersection/inflection axes(FIAs) 

分 类 号：P542[天文地球—构造地质学]