Effects of reactive dissolution of orthopyroxene in producing incompatible element depleted melts and refractory mantle residues during early fore-arc spreading: constraints from ophiolites in eastern Mediterranean-Reference-Cited by-同舟云学术

Effects of reactive dissolution of orthopyroxene in producing incompatible element depleted melts and refractory mantle residues during early fore-arc spreading: constraints from ophiolites in eastern Mediterranean

Published:2020-05 Issue: Volume:360-361 Page:105438
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Aldanmaz Ercan,van Hinsbergen Douwe J.J.,Yıldız-Yüksekol Özlem,Schmidt Max W.,McPhee Peter J.,Meisel Thomas,Güçtekin Aykut,Mason Paul R.D.

Funder

Kocaeli University

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference81 articles.

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3. 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;Aldanmaz;Chem. Geol.,2012

4. Origin and emplacement of the late cretaceous Baer-Bassit ophiolite and its metamorphic sole in NW Syria;Al-Riyami;Lithos,2002

5. Characterisation of spinel peridotites by olivine-spinel compositional relationships: review and interpretation;Arai;Chem. Geol.,1994

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