Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Jeffrey P. Gay"'
Autor:
Jeffrey P. Gay, Estelle E. Ledoux, Matthias Krug, Julien Chantel, Anna Pakhomova, Carmen Sanchez‐Valle, Sergio Speziale, Sébastien Merkel
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 11, Pp n/a-n/a (2024)
Abstract Seismic anisotropy is a powerful tool to map deformation processes in the deep Earth. Below 660 km, however, observations are scarce and conflicting. In addition, the underlying crystal scale mechanisms, leading to microstructures and crysta
Externí odkaz:
https://doaj.org/article/0955158a11a74c208b0fb05bf7fbdbee
Autor:
Estelle E. Ledoux, Morvarid Saki, Jeffrey P. Gay, Matthias Krug, Olivier Castelnau, Wen‐Yi Zhou, Jin S. Zhang, Julien Chantel, Nadège Hilairet, Maxim Bykov, Elena Bykova, Georgios Aprilis, Volodymyr Svitlyk, Gaston Garbarino, Carmen Sanchez‐Valle, Christine Thomas, Sergio Speziale, Sébastien Merkel
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 24, Iss 11, Pp n/a-n/a (2023)
Abstract Wadsleyite is the dominant mineral of the upper portion of the Earth's mantle transition zone (MTZ). As such, understanding plastic deformation of wadsleyite is relevant for the interpretation of observations of seismic signals from this reg
Externí odkaz:
https://doaj.org/article/9b7211ad86a141f5ae169f3492b25db5
Autor:
Matthias Krug, Morvarid Saki, Estelle Ledoux, Jeffrey P. Gay, Julien Chantel, Anna Pakhomova, Rachel Husband, Arno Rohrbach, Stephan Klemme, Christine Thomas, Sébastien Merkel, Carmen Sanchez‐Valle
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 23, Iss 10, Pp n/a-n/a (2022)
Abstract The coesite‐stishovite phase transition is considered the most plausible candidate to explain the X‐discontinuity observed at around 300 km depth in a variety of tectonic settings. Here, we investigate the microstructure in SiO2 across t
Externí odkaz:
https://doaj.org/article/b196574b061a49da82c601ff14c17f93
Autor:
Jeffrey P. Gay, Estelle Ledoux, Matthias Krug, Julien Chantel, Anna Pakhomova, Hanns-Peter Liermann, Carmen Sanchez-Valle, Sébastien Merkel
Publikováno v:
Earth and Planetary Science Letters
Earth and Planetary Science Letters, 2023, Earth and Planetary Science Letters, 604, pp.118015. ⟨10.1016/j.epsl.2023.118015⟩
Earth and planetary science letters 604, 118015 (2023). doi:10.57745/I0J6LZ
Earth and planetary science letters 604, 118015 (2023). doi:10.1016/j.epsl.2023.118015
Earth and Planetary Science Letters, 2023, Earth and Planetary Science Letters, 604, pp.118015. ⟨10.1016/j.epsl.2023.118015⟩
Earth and planetary science letters 604, 118015 (2023). doi:10.57745/I0J6LZ
Earth and planetary science letters 604, 118015 (2023). doi:10.1016/j.epsl.2023.118015
Earth and planetary science letters 604, 118015 (2023). doi:10.1016/j.epsl.2023.118015
The ‘660’ discontinuity is often associated with a phase transitions in pyrolite at about 24 GPa. There are ubiquitous reports of seismic anisotropy below
The ‘660’ discontinuity is often associated with a phase transitions in pyrolite at about 24 GPa. There are ubiquitous reports of seismic anisotropy below
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ff2b467c2cae8c65a1c9c2016abbb931
https://hal.univ-lille.fr/hal-03978933/file/gay2023epsl.pdf
https://hal.univ-lille.fr/hal-03978933/file/gay2023epsl.pdf
