O–H isotope ratios of high pressure ultramafic rocks:...

O–H isotope ratios of high pressure ultramafic rocks: implications for fluid sources and mobility in the subducted hydrous mantle

Gretchen L. Früh-Green, Marco Scambelluri, Franca Vallis
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Volume:
141
Language:
english
Pages:
15
DOI:
10.1007/s004100000228
Date:
May, 2001
File:
PDF, 463 KB
english, 2001
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