Geochemistry and petrology of the Kermanshah ophiolites (Iran): Implication for the interaction between passive rifting, oceanic accretion, and OIB-type components in the Southern Neo-Tethys Ocean-Reference-Cited by-同舟云学术

Geochemistry and petrology of the Kermanshah ophiolites (Iran): Implication for the interaction between passive rifting, oceanic accretion, and OIB-type components in the Southern Neo-Tethys Ocean

Published:2013-07 Issue:1 Volume:24 Page:392-411
ISSN:1342-937X
Container-title:Gondwana Research
language:en
Short-container-title:Gondwana Research

Author:

Saccani Emilio,Allahyari Khalil,Beccaluva Luigi,Bianchini Gianluca

Publisher

Elsevier BV

Subject

Geology

Reference72 articles.

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3. Quantitative models of trace element behavior in magmatic processes;Allègre;Earth and Planetary Science Letters,1978

4. Isotopic evolution of the mantle: the role of magma mixing;Anderson;Earth and Planetary Science Letters,1982

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

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