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Catherine McCammon

Geowissenschaftlerin

Name	Catherine McCammon
Ort	Bayreuth (Wirkungsort) Australien
Geschlecht	weiblich
Beruf	Geowissenschaftlerin (charakteristischer Beruf)
Variante	Catherine A. Mccammon
Beziehung	Bayerisches Forschungsinstitut für Experimentelle Geochemie und Geophysik (Bayreuth) Universität Bayreuth
Weitere Angaben	Promotion 1984 Australian National University Canberra. - Habilitation 2017 Universität Bayreuth. - Seit 1990 Bayerisches Geoinstitut, Universität Bayreuth
Datensatztyp	Person
GND-Nummer	1159395934
Datensatz-ID	1159395934
Beteiligt an alle anzeigen Monoclinic distortion and magnetic transitions in FeO under pressure and temperature Cubic Fe-bearing majorite synthesized at 18–25 GPa and 1000 °C: implications for element transport, subducted slab rheology and diamond formation Efect of faceting on olivine wetting properties Iron and aluminum substitution mechanism in the perovskite phase in the system MgSiO 3 -FeAlO 3 -MgO Crystal chemistry and compressibility of Fe₀.₅Mg₀.₅Al₀.₅Si₀.₅O₃ and FeMg₀.₅Si₀.₅O₃ silicate perovskites at pressures up to 95 GPa Experimental constraints on the ferric Fe content and oxygen fugacity in subducted serpentinites Experimental Constraints on the Ferric Fe Content and Oxygen Fugacity in Subducted Serpentinites Subduction-related oxidation of the sublithospheric mantle evidenced by ferropericlase and magnesiowüstite diamond inclusions Sound Velocity Measurements of B2-Fe-Ni-Si Alloy Under High Pressure by Inelastic X-Ray Scattering : Implications for the Composition of Earth's Core Chemical Stability of FeOOH at High Pressure and Temperature, and Oxygen Recycling in Early Earth History Chemical Stability of FeOOH at High Pressure and Temperature, and Oxygen Recycling in Early Earth History ** Serpentinization-driven H2 production from continental break-up to mid-ocean ridge spreading: unexpected high rates at the West Iberia margin Effects of composition and pressure on electronic states of iron in bridgmanite Seismic detectability of carbonates in the deep Earth: A nuclear inelastic scattering study Deep Earth carbon reactions through time and space Carbonate-silicate reactions at conditions of the Earth’s mantle and the role of carbonates as possible trace-element carriers Stability and Solubility of the FeAlO3 Component in Bridgmanite at Uppermost Lower Mantle Conditions The crystal structures of Fe-bearing MgCO3 sp2- and sp3-carbonates at 98 GPa from single-crystal X-ray diffraction using synchrotron radiation A new (Mg 0.5 F e 0.5 3 + $\begin{array}{} \displaystyle {\rm Fe_{0.5}^{3+}} \end{array}$)(Si 0.5 A l 0.5 3 + $\begin{array}{} \displaystyle {\rm Al_{0.5}^{3+}} \end{array}$) O 3 LiNbO 3 -type phase synthesized at lower mantle conditions Experimental investigation of FeCO 3 (siderite) stability in Earth’s lower mantle using XANES spectroscopy Fe-N system at high pressure reveals a compound featuring polymeric nitrogen chains Oxidized iron in garnets from the mantle transition zone Pressure tuning of charge ordering in iron oxide The high-pressure behavior of spherocobaltite (CoCO3): a single crystal Raman spectroscopy and XRD study Single crystal synthesis of δ-(Al,Fe) OOH The spin state of Fe 3+ in lower mantle bridgmanite Effect of composition on compressibility of skiagite-Fe-majorite garnet Eine NiAs-artige Hochdruckmodifikation von FeN High-Pressure NiAs-Type Modification of FeN Stability of iron-bearing carbonates in the deep Earth’s interior Sound velocities of bridgmanite from density of states determined by nuclear inelastic scattering and first-principles calculations Sound velocities of bridgmanite from density of states determined by nuclear inelastic scattering and first-principles calculations Stability of Fe,Al-bearing bridgmanite in the lower mantle and synthesis of pure Fe-bridgmanite High-pressure spectroscopic study of siderite (FeCO 3) with a focus on spin crossover High-pressure synthesis of skiagite-majorite garnet and investigation of its crystal structure Pressure-induced structural phase transition of the iron end-member of ringwoodite (g-Fe 2 SiO 4) investigated by X-ray diffraction and Mössbauer spectroscopy Oxidation of the Kaapvaal lithospheric mantle driven by metasomatism

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Katalog der Deutschen Nationalbibliothek

Catherine McCammon

Monoclinic distortion and magnetic transitions in FeO under pressure and temperature

Cubic Fe-bearing majorite synthesized at 18–25 GPa and 1000 °C: implications for element transport, subducted slab rheology and diamond formation

Efect of faceting on olivine wetting properties

Iron and aluminum substitution mechanism in the perovskite phase in the system MgSiO 3 -FeAlO 3 -MgO

Crystal chemistry and compressibility of Fe₀.₅Mg₀.₅Al₀.₅Si₀.₅O₃ and FeMg₀.₅Si₀.₅O₃ silicate perovskites at pressures up to 95 GPa

Experimental constraints on the ferric Fe content and oxygen fugacity in subducted serpentinites

Experimental Constraints on the Ferric Fe Content and Oxygen Fugacity in Subducted Serpentinites

Subduction-related oxidation of the sublithospheric mantle evidenced by ferropericlase and magnesiowüstite diamond inclusions

Sound Velocity Measurements of B2-Fe-Ni-Si Alloy Under High Pressure by Inelastic X-Ray Scattering : Implications for the Composition of Earth's Core

Chemical Stability of FeOOH at High Pressure and Temperature, and Oxygen Recycling in Early Earth History

Chemical Stability of FeOOH at High Pressure and Temperature, and Oxygen Recycling in Early Earth History **

Serpentinization-driven H2 production from continental break-up to mid-ocean ridge spreading: unexpected high rates at the West Iberia margin

Effects of composition and pressure on electronic states of iron in bridgmanite

Seismic detectability of carbonates in the deep Earth: A nuclear inelastic scattering study

Deep Earth carbon reactions through time and space

Carbonate-silicate reactions at conditions of the Earth’s mantle and the role of carbonates as possible trace-element carriers

Stability and Solubility of the FeAlO3 Component in Bridgmanite at Uppermost Lower Mantle Conditions

The crystal structures of Fe-bearing MgCO3 sp2- and sp3-carbonates at 98 GPa from single-crystal X-ray diffraction using synchrotron radiation

A new (Mg 0.5 F e 0.5 3 + $\begin{array}{} \displaystyle {\rm Fe_{0.5}^{3+}} \end{array}$)(Si 0.5 A l 0.5 3 + $\begin{array}{} \displaystyle {\rm Al_{0.5}^{3+}} \end{array}$) O 3 LiNbO 3 -type phase synthesized at lower mantle conditions

Experimental investigation of FeCO 3 (siderite) stability in Earth’s lower mantle using XANES spectroscopy

Fe-N system at high pressure reveals a compound featuring polymeric nitrogen chains

Oxidized iron in garnets from the mantle transition zone

Pressure tuning of charge ordering in iron oxide

The high-pressure behavior of spherocobaltite (CoCO3): a single crystal Raman spectroscopy and XRD study

Single crystal synthesis of δ-(Al,Fe) OOH

The spin state of Fe 3+ in lower mantle bridgmanite

Effect of composition on compressibility of skiagite-Fe-majorite garnet

Eine NiAs-artige Hochdruckmodifikation von FeN

High-Pressure NiAs-Type Modification of FeN

Stability of iron-bearing carbonates in the deep Earth’s interior

Sound velocities of bridgmanite from density of states determined by nuclear inelastic scattering and first-principles calculations

Sound velocities of bridgmanite from density of states determined by nuclear inelastic scattering and first-principles calculations

Stability of Fe,Al-bearing bridgmanite in the lower mantle and synthesis of pure Fe-bridgmanite

High-pressure spectroscopic study of siderite (FeCO 3) with a focus on spin crossover

High-pressure synthesis of skiagite-majorite garnet and investigation of its crystal structure

Pressure-induced structural phase transition of the iron end-member of ringwoodite (g-Fe 2 SiO 4) investigated by X-ray diffraction and Mössbauer spectroscopy

Oxidation of the Kaapvaal lithospheric mantle driven by metasomatism