• Site Map

    All the web pages on the conference website







My Goldschmidt

Role functions

All abstracts by Catherine McCammon in conference series: Goldschmidt

An Experimental Approach to a Multiple Saturation Point of a “Direct Ascent” Petit-Spot Basalt
Yutani T, Condamine P, Hirano N, McCammon C & Frost D

The Redox State of Subduction Zones and the Implications for the Speciation of Volatiles
Frost D, Eberhard L, Melai C, Boffa Ballaran T & McCammon C

Magnetism in Iron-Nickel Alloys
McCammon C, Wei Q & Gilder S

(2019) Fe-Mg-Mn Exchange between Olivine and Melt and an Oxybarometer for Basaltic Systems
Blundy J, Melekhova L, Ulmer P, Pichavant M, Humphreys M, Ziberna L, Cerantolo V, Brooker R & McCammon C

(2019) Did Bacteria Induce Redox Cycling of Magnetite within Banded Iron Formations (BIFs)?
Byrne J, Schad M, McCammon C, Tomaszewski E, Smith A, Cerantola V & Kappler A

(2019) The Effect of Oxygen Fugacity on the Stability and Ferric Iron Content of Antigorite
Eberhard L, Frost D & McCammon C

(2019) Ferric Ferrous Ratios in Mantle Xenoliths by Synchrotron Mössbauer Source Spectroscopy
Kiseeva K, Wood B, McCammon C & Ashchepkov I

(2019) Iron Speciation in Olivine-Hosted Melt Inclusions Inferred from Mössbauer Spectroscopy
Gaborieau M, Laubier M, Bolfan-Casanova N, McCammon C, Vantelon D & Chumakov A

(2018) Aiding Atmosphere Oxidation Through Mantle Convection
Lee K, Gu T, Creasy N, Li M, McCammon C & Girard J

(2018) Mantle Metasomatism as Recorded in Diamond Dissolution Features
Fedortchouk Y, Chinn I, Liebske C & McCammon C

(2018) Silicate Melt Ferric/Ferrous Iron Speciation and the Redox State of a Deep Magma Ocean
Frost D, Armstrong K, Rubie D, McCammon C, Boffa Ballaran T, Siersch N & Wang Y

(2018) On the Use of Experimentally Derived Redox Sensors in Olivine-Hosted Melt Inclusions
Laubier M, Bolfan-Casanova N, Gaborieau M & McCammon C

(2017) Facilitating Atmosphere Oxidation Through Mantle Convection
Lee K, Gu T, Creasy N, Li M & McCammon C

(2017) Oxidation State of Majoritic Garnet Inclusions in Diamond
Kiseeva K, Vasiukov D, Wood B, McCammon C, Stachel T, Chumakov A & Dubrovinsky L

(2017) Effect of Composition on Compressibility of skiagite-Fe-Majorite Garnet
Ismailova L, Bykov M, Bykova E, Bobrov A, Dubrovinskaia N, McCammon C & Dubrovinsky L

(2017) Effect of Fe3+ on the Subsolidus and Melting Phase Relations Under Lower Mantle Conditions
Sinmyo R, Nakajima Y, McCammon C, Miyajima N, Petitgirard S, Myhill R & Frost D

(2017) Do Fe-Bearing Minerals Control the Deep Carbon Cycle in the Interior of the Earth?
Stagno V, McCammon CA, Cerantola V, Andreozzi GB, Caruso M, Arimoto T & Irifune T

(2017) Elastic Wave Velocities of Fe-Bearing Carbonates: A Nuclear Inelastic Scattering Study for Deep Carbon
Chariton S, McCammon C, Vasiukov D, Cerantola V, Aprilis G, Chumakov A & Dubrovinsky L

(2016) Transformations of Hydrocarbons during Hot Subduction
Mukhina E, Dubrovinsky L, Serovajskii A, McCammon C, Kolesnikov A, Kupenko I & Kutcherov V

(2016) Evidence for Water in the Lower Mantle from Ferropericlase Included in Diamond
Palot M, Jacobsen SD, Townsend JP, Nestola F, Marquardt K, Harris JW, Stachel T, McCammon CA & Pearson DG

(2016) The Spin State of Fe3+ in Lower Mantle Bridgmanite
Sinmyo R, McCammon C & Dubrovinsky L

(2016) Strong Affinity of Al-Containing Bridgmanite for Ferric Iron
McCammon C, van Driel J, Kawazoe T, Myhill R & Dubrovinsky L

(2016) Stability of Fe, Al-Bearing Bridgmanite in the Lower Mantle and Synthesis of Pure Iron Bridgmanite
Ismailova L, Bykova E, Bykov M, Cerantola V, McCammon C, Boffa Ballaran T, Bobrov A, Dubrovinskaia N & Dubrovinsky L

(2016) Reductive Decomposition of Phase D by Formation of Fe-Bearing Aluminous Bridgmanite
Ishii T, Miyajima N, Petitgirard S, McCammon C & Katsura T

(2016) The Oxidation State of Iron in Silicate Melts as a Function of Pressure
Armstrong K, Frost D, McCammon C, Rubie D & Boffa-Ballaran T

Goldschmidt® is a registered trademark of the Geochemical Society and of the European Association of Geochemistry

Website managed and hosted by White Iron Conferences on behalf of the international geochemical community