 | Mottl, Michael J., Wheat, C. Geoffrey, Fryer, Patricia, Gharib, Jim, Martin, Jonathan B. (2004) Chemistry of springs across the Mariana forearc shows progressive devolatilization of the subducting plate. Geochimica et Cosmochimica Acta, 68 (23) 4915-4933 doi:10.1016/j.gca.2004.05.037 | Journal (article/letter/editorial) | | 2004.05.037 Chemistry of springs across the Mariana forearc shows progressive devolatilization of the subducting...serpentinite mud volcanoes in the outer half of the Mariana forearc provide a unique window into processes of devolatilization...devolatilization of the subducting Pacific Plate. We have sampled upwelling pore waters with lower chlorinity...from 13°47=N to 19°33=N and 52 to 90 km from the Mariana trench axis, corresponding to approximate depths... These systematic variations across the outer forearc imply that the solutions ascend more or less vertically |  | WHEAT, C, FRYER, P, FISHER, A, HULME, S, JANNASCH, H, MOTTL, M, BECKER, K (2008) Borehole observations of fluid flow from South Chamorro Seamount, an active serpentinite mud volcano in the Mariana forearc. Earth and Planetary Science Letters, 267 (3) 401-409 doi:10.1016/j.epsl.2007.11.057 | Journal (article/letter/editorial) | | from South Chamorro Seamount, an active serpentinite mud volcano in the Mariana forearc C. Geoffrey Wheat...on South Chamorro Seamount, an active serpentinite mud volcano in the Mariana forearc to explore subduction-related...from trends in pore water data collected during Ocean Drilling Program Leg 195 when the observatory was...numerous slumps on the southeastern flank of the seamount, and likely shape a geochemical environment suitable...Elsevier B.V. All rights reserved. Keywords: Mariana forearc; mud volcano; CORK; subduction; serpentinite; |  | | Journal (article/letter/editorial) | | slab £uids as inferred from a serpentine seamount, Mariana forearc Laurie D. Benton a;b; *, Je¡rey G. Ryan...clasts and muds erupted from Conical Seamount, Mariana forearc, show substantial enrichment in boron...B-rich pore fluids that are upwelling through the seamount. If the trends of decreasing N11 B with slab depth...suites in the Izu and Kurile arcs of the western Pacific are extended to shallow depths (V25 km), they intersect...B of the slab-derived fluids (+13x) at Conical Seamount. Simple mixtures of a B-rich fluid with a high |  | | Report (issue) | | Precipitation HelmutWeickmann (Ed.) 6 The Crust of the Pacific Basin Gordon A. Macdonald and Hisashi Kuno (Eds...Terranes(IUGG Volume 5) JohnW. Hillhouse(Ed.) Indian Ocean RobertA. Duncan, David K. Rea, (Eds.) 51 Properties...Iijima(Eds.) Flow and Melt Generation at Mid-Ocean Ridges Jason Phipps Morgan,DonnaK. Blackman, andJohnM...Active Margins and Marginal Basins of the Western Pacific Brian Taylor JamesNatland Editors American Geophysical...Active marginsand marginalbasinsof the western Pacific / Taylor. James Natland, editors. p. cm.- (Geophysicalmonograph: |
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