Olivine fabric evolution in a hydrated ductile shear zone at the Moho Transition Zone, Oman Ophiolite-Reference-Cited by-同舟云学术

Olivine fabric evolution in a hydrated ductile shear zone at the Moho Transition Zone, Oman Ophiolite

Published:2013-09 Issue: Volume:377-378 Page:299-310
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Michibayashi Katsuyoshi,Oohara Tatsuya

Publisher

Elsevier BV

Subject

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

Reference85 articles.

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4. High pressure experimental calibration of the olivine–orthopyroxene-spinel oxygen geobarometer: implications for the oxidation state of the upper mantle;Ballhaus;Contrib. Mineral. Petrol.,1991

5. Microstructure and fabric transitions in calcite tectonites from the Sierra Alhamilla (Spain);Behrmann;Geol. Rundsch.,1983

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