O
Oliver T. Lord
Researcher at University of Bristol
Publications - 34
Citations - 1339
Oliver T. Lord is an academic researcher from University of Bristol. The author has contributed to research in topics: Mantle (geology) & Diamond anvil cell. The author has an hindex of 18, co-authored 30 publications receiving 1071 citations. Previous affiliations of Oliver T. Lord include University College London.
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Journal ArticleDOI
Primary carbonatite melt from deeply subducted oceanic crust
Michael J. Walter,Galina Bulanova,Lora S. Armstrong,Shantanu Keshav,Jon D Blundy,Gudmundur H. Gudfinnsson,Oliver T. Lord,A. Lennie,Simon M. Clark,C.B. Smith,Luiz Gobbo +10 more
TL;DR: Experimental and geochemical evidence is provided that silicate mineral inclusions in diamonds from Juina, Brazil, crystallized from primary and evolved carbonatite melts in the mantle transition zone and deep upper mantle.
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Melting in the Fe–C system to 70 GPa
Oliver T. Lord,Michael J. Walter,Rajdeep Dasgupta,Rajdeep Dasgupta,David Walker,Simon M. Clark +5 more
TL;DR: In this article, the authors determined high-pressure melting curves for Fe3C, Fe7C3 and the Fe-Fe3C eutectic using laser-heated diamond anvil cell techniques.
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Equation of state and phase diagram of FeO
Rebecca A. Fischer,Andrew J. Campbell,G. A. Shofner,Oliver T. Lord,Przemyslaw Dera,Vitali B. Prakapenka +5 more
TL;DR: In this paper, Wuestite was mixed with iron metal, which served as the pressure standard, under the assumption that negligible oxygen dissolved into the iron, and X-ray diffraction measurements were performed using a laser-heated diamond anvil cell to achieve simultaneous high pressures and temperatures.
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Fe–FeO and Fe–Fe 3 C melting relations at Earth's core–mantle boundary conditions: Implications for a volatile-rich or oxygen-rich core
Guillaume Morard,Denis Andrault,Daniele Antonangeli,Yoichi Nakajima,Anne-Line Auzende,E. Boulard,S. Cervera,A. N. Clark,Oliver T. Lord,Julien Siebert,Volodymyr Svitlyk,Gaston Garbarino,Mohamed Mezouar +12 more
TL;DR: In this article, the melting properties of the outer core of the Fe-S and Fe-Si systems were investigated using X-Ray diffraction and textural characterisation of recovered samples.
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The FeSi phase diagram to 150 GPa
Oliver T. Lord,Michael J. Walter,David P. Dobson,Lora S. Armstrong,Simon M. Clark,Annette K. Kleppe +5 more
TL;DR: The melting point of FeSi reaches similar to 4000 K at the core mantle boundary and an extrapolated value of 4900 k at the inner core boundary (ICB) as mentioned in this paper.