Sulfide-rich continental roots at cratonic margins formed by carbonated melts. [PDF]
Chen C +7 more
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Machine learning-based identification of key biotic and abiotic drivers of mineral weathering rate in a complex enhanced weathering experiment. [PDF]
Janssens I +19 more
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Low melt viscosity enables melt doublets above the 410-km discontinuity. [PDF]
Xie L +15 more
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Active conversion of atmospheric carbon dioxide to methane in peridotites of the Samail Ophiolite, Oman. [PDF]
Nothaft DB +4 more
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Large melt diversity at a mid-ocean ridge thermal low. [PDF]
Brunelli D +8 more
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Water-rich incipient melt of the deep upper mantle indicates locally preserved low-velocity zones above the 410 km discontinuity. [PDF]
Xie L +4 more
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Slab melting boosts the mantle wedge contribution to Li-rich magmas. [PDF]
Schettino E +9 more
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Decoupling of high-pressure H2 production from serpentinization and magnetite in subduction zones
Siron G +4 more
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This paper presents field, petrographic-structural and geochemical data on spinel and plagioclase peridotites from the southern domain of the Lanzo ophiolitic peridotite massif (Western Alps). Spinel lherzolites, harzburgites and dunites crop out at Mt. Arpone and Mt. Musinè. Field evidence indicates that pristine porphyroclastic spinel lherzolites are
Alberto Zanetti, Othmar Müntener
exaly +6 more sources
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Viscosity of peridotite liquid
Earth and Planetary Science Letters, 2004The Newtonian viscosity of molten peridotite has been determined experimentally at superliquidus and supercooled conditions. The high-temperature determinations were obtained using a concentric cylinder technique employing constant high-speed deformation. The low-temperature determinations have been obtained from the analysis of the glass transition in
Donald B Dingwell +2 more
exaly +2 more sources

