4.4 Article

First occurrence of Fe-Mg-carpholite documenting a high-pressure metamorphism in metasediments of the Lycian Nappes, SW Turkey

Journal

INTERNATIONAL JOURNAL OF EARTH SCIENCES
Volume 89, Issue 4, Pages 867-873

Publisher

SPRINGER
DOI: 10.1007/s005310000103

Keywords

HP-LT metamorphism; carpholite; Lycian nappes; SW Turkey

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In the basal thrust sheets of the Lycian nappes fresh Fe-Mg-carpholite documents low-grade. high-pressure (HP) metamorphism. Here we describe the first occurrences of this HP indicator mineral in Turkey, its regional distribution and geodynamic consequences. Carpholite and its breakdown products, such as chloritiod and pyrophyllite, occur in the Lycian nappes s.s. Relics of Fe-Mg-carpholite were also found in klippen of Lycian nappe material located on top of the Menderes crystalline massif. The distribution of the Fe-Mg-carpholite and its relies traces an extensive area of HP metamorphism in the sediments of a passive continental margin.

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