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pro vyhledávání: '"J. W. DesOrmeau"'
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 25, Iss 3, Pp n/a-n/a (2024)
Abstract Dehydration reactions within subducted oceanic crust are important for fluid‐mediated element transfer within the subducting plate and potentially to the mantle wedge. The effects of metamorphic reactions and fluid flow on element recyclin
Externí odkaz:
https://doaj.org/article/194b7901c655479fbb5d34bac65ef43d