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Full-Text Articles in Physical Sciences and Mathematics
Polymetamorphic Evolution Of The Pan-African Basement And Palaeozoic-Early Tertiary Cover Series Of The Menderes Massif, Osman Candan, Roland Oberhänsli, O. Özcan Dora, Mete Çeti̇nkaplan, O. Ersin Koralay, Gaëtan Rimmelé, Fukun Chen, Cüneyt Akal
Polymetamorphic Evolution Of The Pan-African Basement And Palaeozoic-Early Tertiary Cover Series Of The Menderes Massif, Osman Candan, Roland Oberhänsli, O. Özcan Dora, Mete Çeti̇nkaplan, O. Ersin Koralay, Gaëtan Rimmelé, Fukun Chen, Cüneyt Akal
Bulletin of the Mineral Research and Exploration
The Menderes Massif exposing in the Western Anatolia substantially presents a complex tectonostratigraphy as a result of Late Alpine compressional tectonism. The lithostratigraphical succession of this crystalline complex can be divided into two units: 1- The Pan-African basement (core series) and 2-Palaeozoic - Early Tertiary metasedimentary rocks (cover series). The Pan-African basement of the Menderes Massif is made up of a Late Neoproterozoic metaclastic sequence consisting of paragneisses and conformably overlying micaschists. This high-grade metaclastic sequence is extensively migmatized and intruded by the syn- to post-PanAfrican gabbros and granitoids. The primary contact relationship between the core and cover series is …