High-pressure experiments provide insights into the Mantle Transition Zone history of chromitite in Tibetan ophiolites-Reference-Cited by-同舟云学术

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High-pressure experiments provide insights into the Mantle Transition Zone history of chromitite in Tibetan ophiolites

Published:2017-04 Issue: Volume:463 Page:151-158
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Zhang Yanfei,Jin Zhenmin,Griffin William L.,Wang Chao,Wu Yao

Funder

State Oceanic Administration

National Science Foundation of China

Australian Research Council

GEMOC Key Centre

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference49 articles.

1. The subductibility of continental lithosphere;Afonso,2011

2. High pressure transitions in the system MgAl2O4–CaAl2O4: a new hexagonal aluminous phase with implication for the lower mantle;Akaogi;Phys. Earth Planet. Inter.,1999

3. Origin of podiform chromitites;Arai;J. Asian Earth Sci.,1997

4. Possible recycled origin for ultrahigh-pressure chromitites in ophiolites;Arai;J. Mineral. Petrol. Sci.,2010

5. Conversion of low-pressure chromitites to ultrahigh-pressure chromitites by deep recycling: a good inference;Arai;Earth Planet. Sci. Lett.,2013

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3. Two-pyroxene intergrowth exsolution textures in ophiolitic chromites: implications for the deep mantle origin of the Mirdita ophiolite, Albania;Journal of the Geological Society;2024-01

4. To the transition zone and back: Records from diopside exsolution lamellae in chromite from Archean ophiolitic podiform chromitites;Earth and Planetary Science Letters;2024-01

5. Hpht Experiments on Diamond Crystallization Controlled by Mn-Chromite-Mn-Spinel-Hematite Equilibrium: Implications to Natural Diamonds in Ophiolites;2024

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