Constraints on the evolutionary history of aluminous mafic rocks in the Ronda peridotite massif (Spain) from trace-element compositions of clinopyroxene and garnet-Reference-Cited by-同舟云学术

Constraints on the evolutionary history of aluminous mafic rocks in the Ronda peridotite massif (Spain) from trace-element compositions of clinopyroxene and garnet

Published:2009 Issue:3 Volume:43 Page:191-206
ISSN:0016-7002
Container-title:GEOCHEMICAL JOURNAL
language:en
Short-container-title:Geochem. J.

Author:

MORISHITA TOMOAKI,ARAI SHOJI,ISHIDA YOSHITO,TAMURA AKIHIRO,GERVILLA FERNANDO

Publisher

Geochemical Society of Japan

Subject

Geochemistry and Petrology,Geophysics

Reference73 articles.

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2. Complete mantle section of a slow-spreading ridge-derived ophiolite: An example from the Isabela ophiolite in the Philippines

3. NEW CHEMICAL DATA ON THE CLINOPYROXENE-GARNET PAIR IN THE ALPE ARAMI ECLOGITE, CENTRAL ALPS, SWITZERLAND

4. Origin of Pyroxenite-Peridotite Veined Mantle by Refertilization Reactions: Evidence from the Ronda Peridotite (Southern Spain)

5. Trace elements and Li isotope systematics in Zabargad peridotites: evidence of ancient subduction processes in the Red Sea mantle

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