Biblioteca Digital

61 resultados para Undegassed Mantle

em BORIS: Bern Open Repository and Information System - Berna - Suiça

Highly Refractory Peridotites on Macquarie Island and the Case for Anciently Depleted Domains in the Earth's Mantle

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Plagioclase Peridotites in Ocean-Continent Transitions: Refertilized Mantle Domains Generated by Melt Stagnation in the Shallow Mantle Lithosphere

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Geochemical characteristics and Sr-Nd-Hf isotope compositions of mantle xenoliths and host basalts from Assab, Eritrea: implications for the composition and thermal structure of the lithosphere beneath the Afar Depression

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Mantle wedge peridotites Fossil reservoirs of deep subduction zone processes Inferences from high and ultrahigh-pressure rocks from Bardane (Western Norway) and Ulten (Italian Alps)

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Highly depleted Hadean mantle reservoirs in the sources of early Archean arc-like rocks, Isua supracrustal belt, southern West Greenland

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Makin the Moon from the earth's mantle: the geochemical Perspective

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Evolution of a polymineralic mantle shear zone and the role of second phases in the localization of deformation

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Chromium mobility in hydrous fluids at upper mantle conditions

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A possible high Nb/Ta reservoir in the continental lithospheric mantle and consequences on the global Nb budget - Evidence from continental basalts from Central Germany

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Source of metals in the Guocheng gold deposit, Jiaodong Peninsula, North China Craton: Link to early Cretaceous mafic magmatism originating from Paleoproterozoic metasomatized lithospheric mantle

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Scallop-shaped Depressions and Mantle Sublimation in the Mid-Latitudes of Mars

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HiRISE observations of possible periglacial features in the martian mid-latitude mantle

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Evolution of Mafic Alkaline Melts Crystallized in the Uppermost Lithospheric Mantle: a Melt Inclusion Study of Olivine-Clinopyroxenite Xenoliths Northern Hungary

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Melt-rock reaction processes in the mantle and their bearing on mantle petrology and chemistry (Preface)

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A chemical Earth model with whole mantle convection: the importance of a core-mantle boundary layer (D ) and its early formation

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