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Dissolution of orthopyroxene in basanitic magma between 0.4 and 2 GPa: further implications for the origin of Si-rich alkaline glass inclusions in mantle xenoliths

โœ Scribed by Cliff S. J. Shaw


Publisher
Springer
Year
1999
Tongue
English
Weight
575 KB
Volume
135
Category
Article
ISSN
0010-7999

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