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3He evidence for fluid transfer and continental hydration above a flat slab [期刊论文]
Earth and Planetary Science Letters, 2021-01-01, 556
Hiett C.D.;  Newell D.L.;  Jessup M.J.
View/Download:9/0
 
Elasticity of hydrous ringwoodite at mantle conditions: Implication for water distribution in the lowermost mantle transition zone [期刊论文]
Earth and Planetary Science Letters, 2021-01-01, 554
Wang W.;  Zhang H.;  Brodholt J.P.;  Wu Z.
View/Download:15/0
 
Slab dehydration in warm subduction zones at depths of episodic slip and tremor [期刊论文]
Earth and Planetary Science Letters, 2020-01-01, 552
Condit C.B.;  Guevara V.E.;  Delph J.R.;  French M.E.
View/Download:6/0
 
Hydration of the crust and upper mantle of the Hikurangi Plateau as it subducts at the southern Hikurangi margin [期刊论文]
Earth and Planetary Science Letters, 2020-01-01, 541
Herath P.;  Stern T.A.;  Savage M.K.;  Bassett D.;  Henrys S.;  Boulton C.
View/Download:5/0
 
Fluid-mediated carbon release from serpentinite-hosted carbonates during dehydration of antigorite-serpentinite in subduction zones [期刊论文]
Earth and Planetary Science Letters, 2020-01-01, 531
Menzel M.D.;  Garrido C.J.;  López Sánchez-Vizcaíno V.
View/Download:2/0
 
Fracture-mediated deep seawater flow and mantle hydration on oceanic transform faults [期刊论文]
Earth and Planetary Science Letters, 2020-01-01, 532
Prigent C.;  Warren J.M.;  Kohli A.H.;  Teyssier C.
View/Download:4/0
 
Ps mantle transition zone imaging beneath the Colorado Rocky Mountains: Evidence for an upwelling hydrous mantle [期刊论文]
Earth and Planetary Science Letters, 2018-01-01, 492
Zhang Z.;  Dueker K.G.;  Huang H.-H.
View/Download:1/0
 
An upper bound on the electrical conductivity of hydrated oceanic mantle at the onset of dehydration melting [期刊论文]
Earth and Planetary Science Letters, 2018-01-01, 482
Naif S.
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Assessing the Role of Water in Cordilleran Flat Slab Subduction Regions [项目]
Ryan Porter
View/Download:1/0
 
High-pressure and Temperature Elasticity and Equation of State of Hydrous Phase [项目]
Mainak Mookherjee
View/Download:1/0
 

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