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Chromitites in ophiolites: How, where, when, why? Part II. The crystallization of chromitites

  • Published:2014-02 Issue: Volume:189 Page:140-158
  • ISSN:0024-4937
  • Container-title:Lithos
  • language:en
  • Short-container-title:Lithos

Author:

González-Jiménez José María,Griffin William L.,Proenza Joaquín A.,Gervilla Fernando,O'Reilly Suzanne Y.,Akbulut Mehmet,Pearson Norman J.,Arai Shoji

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference180 articles.

1. Unexpectedly high-PGE chromitite from the deeper mantle section of the northern Oman ophiolite and its tectonics implications;Ahmed;Contributions to Mineralogy and Petrology,2002

2. Osmium isotope systematics of the Proterozoic and Phanerozoic ophiolitic chromitites: in situ ion probe analysis of primary Os-rich PGM;Ahmed;Earth and Planetary Science Letters,2006

3. In-situ Os isotopes in abyssal peridotites bridge the isotopic-gap between MORBs and their source mantle;Alard;Nature,2005

4. Control of wall-rock composition on the formation of podiform chromitites as a result of magma/peridotite interaction;Arai;Resource Geology,1997

5. Possible recycled origin for ultrahigh-pressure chromitites in ophiolites;Arai;Journal of Mineralogical and Petrological Sciences,2010
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