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Experimental evidence supports mantle partial melting in the asthenosphereLattice thermal conductivity of lower mantle minerals and heat flux from Earth's core.Dehydration of chlorite explains anomalously high electrical conductivity in the mantle wedges.Experimental evidence supporting a global melt layer at the base of the Earth's upper mantle.Single crystal elasticity of natural topaz at high-temperatures.Low hydrogen contents in the cores of terrestrial planets.Argon behavior in basaltic melts in presence of a mixed H 2 O-CO 2 fluid at upper mantle conditionsEffect of H 2 O on metal–silicate partitioning of Ni, Co, V, Cr, Mn and Fe: Implications for the oxidation state of the Earth and MarsHot mantle geotherms stabilize calcic carbonatite magmas up to the surfaceDry mantle transition zone inferred from the conductivity of wadsleyite and ringwooditeElectrical conductivity anisotropy in partially molten peridotite under shear deformationElectrical conductivity measurements of periclase under high pressure and high temperatureElectrical conductivity of olivine, wadsleyite and ringwooditeElectrical conductivity of the major upper mantle minerals: a reviewFormation of bridgmanite-enriched layer at the top lower-mantle during magma ocean solidification
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description
forsker
@nb
onderzoeker
@nl
researcher, ORCID id # 0000-0001-8161-081X
@en
name
G. Manthilake
@ast
G. Manthilake
@nl
Geeth Manthilake
@en
Geeth Manthilake
@nb
type
label
G. Manthilake
@ast
G. Manthilake
@nl
Geeth Manthilake
@en
Geeth Manthilake
@nb
altLabel
G. Manthilake
@en
prefLabel
G. Manthilake
@ast
G. Manthilake
@nl
Geeth Manthilake
@en
Geeth Manthilake
@nb
P106
P31
P496
0000-0001-8161-081X