Evidence from accreted seamounts for a depleted component in the early Galapagos plume
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Volatiles in Basaltic Glasses from Loihi Seamount, Hawaii: Evidence for a Relatively Dry Plume Component
New H2O, CO2 and S concentration data for basaltic glasses from ‘hotspot’, with temperature differences of 200°C or more between hotter upwelling plumes and the ambient mantle Loihi seamount, Hawaii, allow us to model degassing, assimilation, adiabat (e.g. White & McKenzie, 1989; Campbell, 1998; and the distribution of major volatiles within and around the Davies, 1998). In contrast, it has lon...
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ژورنال
عنوان ژورنال: Geology
سال: 2016
ISSN: 0091-7613,1943-2682
DOI: 10.1130/g37618.1