Olivine-Ringwoodite Transformation Kinetics Suggest that the Deep Marianas and Pacific Slabs have less than 90 ppm H2O

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ADS bibcode
2007AGUFMDI53A1104D
year
2007
Listed Authors
Du Frane, W. L.
Sharp, T. G.
Leinenweber, K.
Listed Institutions
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-
Arizona State University, ASU School of Earth and Space Exploration PO Box 871404, Tempe, AZ 85287-1404, United States

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