Member Since 2014
Elizabeth Colette Thompson
Assistant Professor, Sewanee The University of the South
AGU Research
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First-principles investigations of antigorite polysomatism under pressure
AGU 2024
mineral and rock physics | 10 december 2024
Jun Tsuchiya, Taiga Mizoguchi, Sayako Inoue, Eliza...
Antigorite is the high-temperature member of the serpentine group minerals and is broadly considered a primary carrier of water in the subducting ocea...
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First‐Principles Investigations of Antigorite Polysomatism Under Pressure
JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH
01 june 2024
Jun Tsuchiya, Taiga Mizoguchi, Sayako Inoue, Eliza...
Antigorite is the high‐temperature member of the serpentine group minerals and is broadly considered a primary carrier of water in the subduc...
Hot and Cold Hydrous Sulfates: Phase Transitions in Epsomite and Melanterite at Elevated Pressures and Extreme Temperatures
PROPERTIES OF VOLATILES AND METAL ALLOYS IN ROCKY PLANETARY INTERIORS AND THEIR SURFACE EXPRESSION III POSTER
mineral and rock physics | 14 december 2022
Máté Garai, Brian Gulick, Christian Shushok, Audre...
Magnesium hydrous sulfates (MgSO4·nH2O) have been identified in chondritic meteorites, on the surface of Mars, and likely form from the coexisten...
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FeOOH Polymorphs in the Deep Earth: Combining Theoretical and Experimental Approaches
EARTH AND PLANETARY MATERIALS: PROPERTIES, INTERACTIONS, AND CONSEQUENCES FOR PLANETARY DYNAMICS I ORAL
mineral and rock physics | 14 december 2021
Elizabeth C. Thompson, Zhenxian Liu, Jun Tsuchiya,...
Our understanding of the Earths interior hinges on knowing where and how hydrogen is stored in the deep Earth because hydrogen has an outsized influen...
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Elastic Properties of the Pyrite‐Type FeOOH‐AlOOH System From First‐Principles Calculations
GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS
11 may 2021
Elizabeth C. Thompson, Andrew Campbell, Jun Tsuchi...
The stability, structure, and elastic properties of pyrite‐type (FeS2 structured) FeO2H were determined using density functional theory‐...
Phase transitions in ε-FeOOH at high pressure and ambient temperature
DECIPHERING THE STRUCTURE, MINERALOGY, AND COMPOSITION OF THE LOWER MANTLE II POSTERS
study of earth's deep interior | 09 december 2020
Elizabeth C. Thompson, Anne Davis, Nigel Brauser, ...
Constraining the accommodation, distribution, and circulation of hydrogen in the Earth’s interior is vital to our broader understanding of the deep Ea...
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Evolution of the crystal structure of hydrous wadsleyite at high pressure up to 33 GPa
MANTLE EVOLUTION, DYNAMICS, CHEMISTRY, AND THE ROLE OF THE TRANSITION ZONE II POSTERS
study of earth's deep interior | 07 december 2020
Fei Wang, Elizabeth C. Thompson, Dongzhou Zhang, J...
Wadsleyite (beta-Mg2SiO4) is thought to be the dominant silicate mineral in the upper part of the transition zone from about 410 to 520 km depth. Whil...
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Changes in hydrogen bonding in wadsleyite at concurrent P-T conditions relevant to encapsulation as inclusion in diamond
CARBON, HYDROGEN, AND VOLATILES INSIDE THE EARTH, PLANETARY BODIES, AND EXOPLANETS II POSTERS
mineral and rock physics | 12 december 2019
Elizabeth C. Thompson, Fei Wang, Zhenxian Liu, Ste...
The discovery of a hydrous ringwoodite diamond inclusion [1] informs our understanding of the deep Earth water cycle, but also raises two compelling q...
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