Please use this identifier to cite or link to this item:
https://hdl.handle.net/20.500.13091/5714
Title: | Crystallisatıon Conditions of Igneous Epidote in a Metamorphıc Sole from Neotethyan Ophiolitic Melange, Konya, Central Southern Turkey | Authors: | Koçak, Kerim Kaya, Raziye Merve |
Keywords: | Igneous Epidote Ophiolite Metamorphic Sole Turkey |
Publisher: | GEOBALCANICA | Abstract: | Subhedral to euhedral epidote occurs with compositional and sector zoning in a metamorphic sole at the bottom of a Neotethyan ophiolitic mélange. The epidote is characterised by low Fe2O3 (5–8%) , high Al2O3 (26-30 %), and minor TiO2 (0.05-0.18 wt%), MnO (0.01-0.1 wt%) and MgO (0-0.12 wt%) contents. Petrographical and mineralogical characteristics and various aluminium-in- hornblende geobarometry estimates suggest that the amphibole associated with epidote was possibly crystallized from a wet tholeiitic/alkaline magma between ~3.5-7 kb pressure conditions. | URI: | https://hdl.handle.net/20.500.13091/5714 |
Appears in Collections: | Mühendislik ve Doğa Bilimleri Fakültesi Koleksiyonu |
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GBP.2019.07.pdf | 398.23 kB | Adobe PDF | View/Open |
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