Dry mantle transition zone inferred from the conductivity of wadsleyite and ringwoodite
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Hydrous mantle transition zone indicated by ringwoodite included within diamond.A nearly water-saturated mantle transition zone inferred from mineral viscosity.Experimental evidence supporting a global melt layer at the base of the Earth's upper mantle.CaSiO3 Perovskite May Cause Electrical Conductivity Jump in the Topmost Lower MantleHigh-P/T experimental studies and water in the silicate mantleElectrical conductivity of orthopyroxene and plagioclase in the lower crustEffect of water on the electrical conductivity of lower crustal clinopyroxeneHydrogen self-diffusivity in single crystal ringwoodite: Implications for water content and distribution in the mantle transition zoneToward a unified hydrous olivine electrical conductivity lawLithospheric dismemberment and magmatic processes of the Great Basin-Colorado Plateau transition, Utah, implied from magnetotellurics
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Dry mantle transition zone inferred from the conductivity of wadsleyite and ringwoodite
description
article publié dans la revue scientifique Nature
@fr
scientific article published in Nature
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wetenschappelijk artikel
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наукова стаття, опублікована в Nature в січні 2008
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name
Dry mantle transition zone inferred from the conductivity of wadsleyite and ringwoodite
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Dry mantle transition zone inferred from the conductivity of wadsleyite and ringwoodite
@nl
type
label
Dry mantle transition zone inferred from the conductivity of wadsleyite and ringwoodite
@en
Dry mantle transition zone inferred from the conductivity of wadsleyite and ringwoodite
@nl
prefLabel
Dry mantle transition zone inferred from the conductivity of wadsleyite and ringwoodite
@en
Dry mantle transition zone inferred from the conductivity of wadsleyite and ringwoodite
@nl
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Dry mantle transition zone inferred from the conductivity of wadsleyite and ringwoodite
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Takuya Matsuzaki
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10.1038/NATURE06427
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2008-01-01T00:00:00Z
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1028430624