Zobrazeno 1 - 10
of 17
pro vyhledávání: '"Hélène Couvy"'
Autor:
Hélène Couvy, Max Eisele, Justin Filiberto, Michael J. Krawczynski, Cosette Dwyer, Ryan C. Ogliore
Publikováno v:
Applied Spectroscopy. 73:767-773
We report an infrared (IR) spectroscopic technique to detect quartz grains with large isotope anomalies. We synthesized isotopically doped quartz and used Fourier transform infrared spectroscopy (FT-IR) in two different instruments: a traditional far
Publikováno v:
Journal of Geophysical Research: Solid Earth. 125
Mylonites are ubiquitous structural features of dynamic plate boundaries, and are widely assumed to represent the product of localized deformation at high pressure and temperature. There are two features of mylonites that distinguish them from typica
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8087374a783a37ee04a6dc79c98df99d
https://doi.org/10.5194/egusphere-egu2020-2672
https://doi.org/10.5194/egusphere-egu2020-2672
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
M. Roskosz, N. X. Nie, Hélène Couvy, Michael Y. Hu, Kelsey B. Prissel, Michael J. Krawczynski, E. Ercan Alp, Nicolas Dauphas
Publikováno v:
Geochimica et Cosmochimica Acta. 238:580-598
Olivine is the most abundant mantle mineral at depths relevant to oceanic crust production through melting. It is also a liquidus phase for a wide range of mafic and ultramafic magma compositions. We have experimentally investigated the effects of ol
Publikováno v:
Scripta Materialia. 64:1019-1022
We present the measurement of the Young’s modulus ( E ) of a nanopolycrystalline diamond (NPD) sample synthesized by the direct conversion of graphite under high pressure and temperature. E has been measured along with the nanohardness ( H N ) usin
Publikováno v:
Physics of the Earth and Planetary Interiors. 177:122-129
Steady-state deformation experiments were carried out in a deformation-DIA (D-DIA) high-pressure apparatus on oriented diopside single crystals, at pressure (P) ranging from 3.8 to 8.8 GPa, temperature (T) from 1100 to 1400 C, and differential stress
Publikováno v:
Physics and Chemistry of Minerals. 37:343-351
We established an equation of state for nanocrystalline forsterite using multi-anvil press and diamond anvil cell. Comparative high-pressure and high-temperature experiments have been performed up to 9.6 GPa and 1,300°C. We found that nanocrystallin
Autor:
Tamás Ungár, Hélène Couvy, Florian Heidelbach, Stephen J. Mackwell, Krisztián Nyilas, Daniel J. Frost, Patrick Cordier
Publikováno v:
European Journal of Mineralogy. 16:877-889
Synthetic forsterite samples were shear-deformed at 11 GPa, 1400°C in the multianvil apparatus. The deformation microstructures have been characterised by SEM, EBSD, X-ray diffraction peak broadening and strain anisotropy analysis, and TEM. Differen