Supra-subduction zone mantle peridotites in the Tethyan Ocean (East Anatolian Accretionary Complex–Eastern Turkey): Petrological evidence for melting and melt-rock interaction-Reference-Cited by-同舟云学术

Supra-subduction zone mantle peridotites in the Tethyan Ocean (East Anatolian Accretionary Complex–Eastern Turkey): Petrological evidence for melting and melt-rock interaction

Published:2021-08-26 Issue:6 Volume:115 Page:663-685
ISSN:0930-0708
Container-title:Mineralogy and Petrology
language:en
Short-container-title:Miner Petrol

Author:

Üner Tijen^ORCID

Funder

Yüzüncü Yil Üniversitesi

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

https://link.springer.com/content/pdf/10.1007/s00710-021-00760-0.pdf

Reference106 articles.

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2. Açlan M, Oyan V, Köse O (2020) Petrogenesis and the evolution of Pliocene Timar basalts in the east of Lake Van, Eastern Anatolia, Turkey: A consequence of the partial melting of a metasomatized spinel–rich lithospheric mantle source. J Afr Earth Sci 168:103844

3. Akmaz RM, Uysal İ, Saka S (2014) Compositional variations of chromite and solid inclusions in ophiolitic chromitites from the southeastern Turkey: Implications for chromitite genesis. Ore Geol Rev 58:208–224

4. Aldanmaz E, Meisel T, Çelik ÖF, Henjes-Kunst F (2012) Osmium isotope systematics and highly siderophile element fractionation in spinel-peridotites from the Tethyan ophiolites in SW Turkey: implications for multi-stage evolution of oceanic upper mantle. Chem Geol 294–295:152–164

5. Arai S (1994) Compositional variation of olivine-chromian spinel in Mg-rich magmas as a guide to their residual spinel peridotites. J Volcanol Geotherm Res 59:279–293

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