Results 171 to 180 of about 39,591 (263)
Copper isotopes track the Neoproterozoic oxidation of cratonic mantle roots. [PDF]
Chen C, Foley SF, Shcheka SS, Liu Y.
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Mineral carbonation of peridotite fueled by magmatic degassing and melt impregnation in an oceanic transform fault. [PDF]
Klein F +8 more
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Anomaly Field Extraction Based on Layered-Earth Model and Equivalent Eddy Current Inversion: A Case Study of Borehole zk506 in Baishiquan, Xinjiang. [PDF]
Yang Y +7 more
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Linking carbonatites, rare earth ores, and subduction-fertilized mantle lithosphere. [PDF]
Spandler C, Merdith AS, Griffin A.
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Incipient carbonate melting drives metal and sulfur mobilization in the mantle. [PDF]
Ezad IS +6 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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Melting of Peridotite to 140 Gigapascals
Science, 2010Under Pressure In order to understand the behavior of materials in the solid deep Earth, it is important to be able to estimate how a material melts at high pressure. To this end, Fiquet et al. (p.
Fiquet, G. +6 more
openaire +3 more sources
Lithos, 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
Piccardo GB, Zanetti A, Müntener O
exaly +4 more sources
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
Piccardo GB, Zanetti A, Müntener O
exaly +4 more sources
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
Daniele Giordano
exaly +2 more sources

