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Michael W. Förster, Yannick Bussweiler, Dejan Prelevic, Nathan R. Daczko, Stephan Buhre, Regina Mertz-Kraus and Stephen F. Foley
Subduction of oceanic crust buries an average thickness of 300?500 m of sediment that eventually dehydrates or partially melts. Progressive release of fluid/melt metasomatizes the fore-arc mantle, forming serpentinite at low temperatures and phlogopite-b...
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P. McNeely, H.-D. Falter, U. Fantz, P. Franzen, M. Fröschle, B. Heinemann, W. Kraus, Ch. Martens, R. Riedl, and E. Speth
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Pike, S. M. Heinz, R. Walk, T. Jones, C. Kraus, G. A. Gassmann, W. Novacky, A. J. Niblack, T. L.
Pág. 456 - 496
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