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Hornblende, cummingtonite, and biotite hydrogen isotopes: Direct evidence of slab-derived fluid flux in silicic magmas of the Taupo Volcanic Zone, New Zealand

✍ Scribed by C.D. Deering; T.W. Horton; D.M. Gravley; J.W. Cole


Book ID
113769987
Publisher
Elsevier Science
Year
2012
Tongue
English
Weight
526 KB
Volume
233-234
Category
Article
ISSN
0377-0273

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