Transformation mechanisms of San Carlos olivine to (MgFe)2SiO4 β-phase under subduction zone conditions
- 31 October 1994
- journal article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 86 (1-3) , 45-67
- https://doi.org/10.1016/0031-9201(94)05061-9
Abstract
No abstract availableKeywords
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