The Beni Bousera Peridotite(Rif Belt, Morocco): A Subsolidus Evolution Interpretation

作     者：MOURABIT Zahra TABIT Abdelhalim ALGOUTI Ahmed ALGOUTI Abdellah 

作者机构：University of Cadi Ayyad Faculty of Science Semlalia Laboratory: Geology of Sedimentary Moroccan BasinsDepartment of Geology 

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

年 卷 期：2016年第90卷第S1期

页      面：111-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：The Beni Bousera Peridotite A Subsolidus Evolution Interpretation Morocco Rif Belt 

摘      要：The Beni Bousera ultramafic massif is a tectonically emplaced body of upper mantle material that is exposed over 72 km2at the base of the internal zones of the Alpine Rif belt of northern *** predominant lithology in