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Autor:
Friederike C. Warkus, Osman Candan, Roland Oberhänsli, S. Dürr, Mete Çetinkaplan, Julius Partzsch, O. Özcan Dora
Publikováno v:
International Journal of Earth Sciences. 89:793-811
The Menderes Massif is made up of Pan-African basement and a Paleozoic to Early Tertiary cover sequence imbricated by Late Alpine deformation. The Precambrian basement comprises primarily medium- to high-grade schists, paragneisses, migmatites, ortho
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5d0561c5d30d9d8dac66cd077a833b5e
https://doi.org/10.1007/s005310000097
https://doi.org/10.1007/s005310000097
