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Year 2019, , 167 - 172, 30.09.2019
https://doi.org/10.17350/HJSE19030000143

Abstract

Chemical and Mineralogical Characteristics of the Microscopic-sized Epidotes in the Metamorphic Basement Rocks within the Late Cretaceous Hatip Ophiolitic Melange in Konya Central Southern Turkey

Year 2019, , 167 - 172, 30.09.2019
https://doi.org/10.17350/HJSE19030000143

Abstract

A metamorphism in green-schist facies conditions. The epidote crystals is subhedral to eu- hedral, with high Al2O3 26-30 % and low Fe2O3 5–8% contents. It is predominantly zoisite Xcz = 0.46 to 0.72 and subordinate epidote Xep =0.27-0.53 in composition, with typical compositional zoning due to variable substitution of Fe3+ and Al3+ on octahedral sites and sector-zoning. The epidote is suggested to have a possible igneous origin, and to be crystallised from a wet H2O>5 wt % magma under low fO2 and intermediate pres- sure conditions during initial stage crystallisation on the basis of its petrographical and mineralogical characteristics

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Details

Primary Language English
Journal Section Research Article
Authors

Kerim Kocak This is me

Raziye Merve Kaya This is me

Publication Date September 30, 2019
Published in Issue Year 2019

Cite

Vancouver Kocak K, Kaya RM. Chemical and Mineralogical Characteristics of the Microscopic-sized Epidotes in the Metamorphic Basement Rocks within the Late Cretaceous Hatip Ophiolitic Melange in Konya Central Southern Turkey. Hittite J Sci Eng. 2019;6(3):167-72.

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