Elastic wave velocities of forsterite and its β‐spinel form and chemical boundary hypothesis for the 410‐km discontinuity
- 10 May 1998
- journal article
- review article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Solid Earth
- Vol. 103 (B5) , 9591-9608
- https://doi.org/10.1029/98jb00024
Abstract
No abstract availableKeywords
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