Results 161 to 170 of about 8,250 (222)

Sulfide-rich continental roots at cratonic margins formed by carbonated melts. [PDF]

open access: yesNature
Chen C   +7 more
europepmc   +1 more source

Machine learning-based identification of key biotic and abiotic drivers of mineral weathering rate in a complex enhanced weathering experiment. [PDF]

open access: yesOpen Res Eur
Janssens I   +19 more
europepmc   +1 more source

Low melt viscosity enables melt doublets above the 410-km discontinuity. [PDF]

open access: yesNat Commun
Xie L   +15 more
europepmc   +1 more source

Large melt diversity at a mid-ocean ridge thermal low. [PDF]

open access: yesSci Adv
Brunelli D   +8 more
europepmc   +1 more source

Slab melting boosts the mantle wedge contribution to Li-rich magmas. [PDF]

open access: yesSci Rep
Schettino E   +9 more
europepmc   +1 more source

Melt/peridotite interaction in the Southern Lanzo peridotite: Field, textural and geochemical evidence

open access: yesLithos, 2007
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, 2004
The 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

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