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Carmen Sanchez-Valle (1976-)

Mineralogin

Name	Carmen Sanchez-Valle
Zeit	1976- (Lebensdaten)
Ort	Münster (Westf) (Wirkungsort) Sonstiges Ausland / Unbekanntes Land
Akademischer Grad bzw. Titel	Prof. Dr.
Beruf	Mineralogin (charakteristischer Beruf) Hochschullehrerin
Variante	C. Sanchez-Valle
Beziehung	Universität Münster
Weitere Angaben	Professorin für Mineralogie am Institut für Mineralogie der WWU Münster
Quelle	https://www.uni-muenster.de/Mineralogie/en/personen/sanchezvalle.shtml (Stand: 30.09.2024)
Datensatztyp	Person
GND-Nummer	1089488408
Datensatz-ID	1089488408
Beteiligt an alle anzeigen Phase transition kinetics of superionic H2O ice phases revealed by Megahertz X-ray free-electron laser-heating experiments Monoclinic distortion and magnetic transitions in FeO under pressure and temperature Automated pipeline processing X-ray diffraction data from dynamic compression experiments on the Extreme Conditions Beamline of PETRA III Optical properties of (Mg,Fe)O at high pressure In-situ study of microstructures induced by the olivine to wadsleyite transformation at conditions of the 410 km depth discontinuity Preferential mobilisation of oxidised iron by slab-derived hydrous silicate melts Rapid compression experiments on quartz and implications for transitions to metastable high-pressure phases Textures Induced by the Coesite-Stishovite Transition and Implications for the Visibility of the X-Discontinuity Bromine speciation and partitioning in slab-derived aqueous fluids and silicate melts and implications for halogen transfer in subduction zones Investigating the effect of the compression rate on the kinetic response of diamond anvil cell experiments Bromine speciation and partitioning in slab-derived fluids and melts: Implications for halogens recycling in subduction zones Bromine speciation and partitioning in slab-derived aqueous fluids and silicate melts and implications for halogen transfer in subduction zones Letter. Densified glasses as structural proxies for high-pressure melts: Configurational compressibility of silicate melts retained in quenched and decompressed glasses Fluids in the Crust. Constraints on the mobilization of Zr in magmatic-hydrothermal processes in subduction zones from in situ fluid-melt partitioning experiments Compositional dependent compressibility of dissolved water in silicate glasses

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Carmen Sanchez-Valle (1976-)

Phase transition kinetics of superionic H2O ice phases revealed by Megahertz X-ray free-electron laser-heating experiments

Monoclinic distortion and magnetic transitions in FeO under pressure and temperature

Automated pipeline processing X-ray diffraction data from dynamic compression experiments on the Extreme Conditions Beamline of PETRA III

Optical properties of (Mg,Fe)O at high pressure

In-situ study of microstructures induced by the olivine to wadsleyite transformation at conditions of the 410 km depth discontinuity

Preferential mobilisation of oxidised iron by slab-derived hydrous silicate melts

Rapid compression experiments on quartz and implications for transitions to metastable high-pressure phases

Textures Induced by the Coesite-Stishovite Transition and Implications for the Visibility of the X-Discontinuity

Bromine speciation and partitioning in slab-derived aqueous fluids and silicate melts and implications for halogen transfer in subduction zones

Investigating the effect of the compression rate on the kinetic response of diamond anvil cell experiments

Bromine speciation and partitioning in slab-derived fluids and melts: Implications for halogens recycling in subduction zones

Bromine speciation and partitioning in slab-derived aqueous fluids and silicate melts and implications for halogen transfer in subduction zones

Letter. Densified glasses as structural proxies for high-pressure melts: Configurational compressibility of silicate melts retained in quenched and decompressed glasses

Fluids in the Crust. Constraints on the mobilization of Zr in magmatic-hydrothermal processes in subduction zones from in situ fluid-melt partitioning experiments

Compositional dependent compressibility of dissolved water in silicate glasses