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Stanislav V. Sinogeikin

Researcher at Carnegie Institution for Science

Publications -  145
Citations -  6071

Stanislav V. Sinogeikin is an academic researcher from Carnegie Institution for Science. The author has contributed to research in topics: Elastic modulus & Brillouin Spectroscopy. The author has an hindex of 45, co-authored 143 publications receiving 5320 citations. Previous affiliations of Stanislav V. Sinogeikin include University of Illinois at Urbana–Champaign & Argonne National Laboratory.

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Sound velocities and elastic properties of γ-Mg2SiO4 to 873 K by Brillouin spectroscopy

TL;DR: In this article, sound velocities and single-crystal elastic moduli of spinel-structured γ-Mg_2SiO_4 were measured to 873 K by Brillouin spectroscopy using a new high-temperature cell designed for singlecrystal measurements.
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Structure of siderite FeCO3 to 56 GPa and hysteresis of its spin-pairing transition

TL;DR: The structure of siderite was determined to 56 GPa, beyond the spin-pairing transition of its iron $d$ electrons as discussed by the authors, which is concomitant with a shrinkage of the octahedral bond distance by 4%, and a volume collapse of 10%.
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Brillouin scattering study on the single-crystal elastic properties of natrolite and analcime zeolites

TL;DR: The Brillouin light-scattering technique was used to investigate the single-crystal elastic properties of two aluminosilicate zeolites, natrolite (NAT) and analcime (ANA), at ambient conditions as mentioned in this paper.
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The laser micro-machining system for diamond anvil cell experiments and general precision machining applications at the High Pressure Collaborative Access Team

TL;DR: Though initially designed mainly for machining of the diamond anvil cell gaskets, the laser-machining system has since found many other micro-Machining applications, several of which are presented here.
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Elastic properties of hydrous ringwoodite

TL;DR: In this article, the authors show that water has a smaller effect on the elastic moduli and velocities of ringwoodite than implied by previous studies, which is consistent with systematic relationships between changes in the elastic properties and density that accompany the hydration of mineral phases.