Mid-ocean ridge and supra-subduction geochemical signatures in spinel–peridotites from the Neotethyan ophiolites in SW Turkey: Implications for upper mantle melting processes-Reference-Cited by-同舟云学术

Mid-ocean ridge and supra-subduction geochemical signatures in spinel–peridotites from the Neotethyan ophiolites in SW Turkey: Implications for upper mantle melting processes

Published:2009-12 Issue:3-4 Volume:113 Page:691-708
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Aldanmaz E.,Schmidt M.W.,Gourgaud A.,Meisel T.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference53 articles.

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3. An estimation of the least depleted spinel peridotite on the basis of olivine–spinel mantle array;Arai;Neues Jahrbuch fur Mineralogie Monatshefte,1987

4. Characterisation of spinel peridotites by olivine–spinel compositional relationships: review and interpretation;Arai;Chemical Geology,1994

5. Trace element modeling of aqueous fluid–peridotite interaction in the mantle wedge of subduction zones;Ayers;Contributions to Mineralogy and Petrology,1998

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