Zobrazeno 1 - 10
of 20
pro vyhledávání: '"M. A. Bouhifd"'
Autor:
M. A. Bouhifd
Publikováno v:
History of Geo- and Space Sciences, Vol 12, Pp 95-96 (2021)
Externí odkaz:
https://doaj.org/article/7c83cadb47344d4b92f33c371da31eaf
Autor:
D. Freitas, G. Manthilake, F. Schiavi, J. Chantel, N. Bolfan-Casanova, M. A. Bouhifd, D. Andrault
Publikováno v:
Nature Communications, Vol 8, Iss 1, Pp 1-7 (2017)
A 56–60 km thick low velocity layer exists at the base of the Earth’s upper mantle. Here, the authors experimentally reproduced the wadsleyite-to-olivine transition in the upwelling mantle and show that the low velocity anomaly can be explained b
Externí odkaz:
https://doaj.org/article/bb8176cb80b04466a94288acf11464e4
Autor:
A. D. Rosa, I. Kupenko, J.-A. Hernandez, A. Forestier, M. Muñoz, G. Morard, M. A. Bouhifd, K. A. Lomachenko, R. Torchio, A. Chumakov, O. Mathon, M. Mezouar
Publikováno v:
Synchrotron Radiation News. 35:8-16
Publikováno v:
Physics and Chemistry of Minerals
Physics and Chemistry of Minerals, 2022, 49, ⟨10.1007/s00269-021-01174-2⟩
Physics and Chemistry of Minerals, 2022, 49, ⟨10.1007/s00269-021-01174-2⟩
co-auteur étranger; International audience; The additional work we have done using our new laser heating in the diamond anvil cell system since the publication of Andrault et al. (Phys Chem Mineral 47(2), 2020) leads us to the conclusion that there
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::309b203ef71005154a23bf5cd3ab3c8e
https://hal-insu.archives-ouvertes.fr/insu-03708909/file/__Melting-SiO2_Corr_v2.pdf
https://hal-insu.archives-ouvertes.fr/insu-03708909/file/__Melting-SiO2_Corr_v2.pdf
Autor:
A. D. Rosa, A. Dewaele, G. Garbarino, V. Svitlyk, G. Morard, F. De Angelis, M. Krstulović, R. Briggs, T. Irifune, O. Mathon, M. A. Bouhifd
Publikováno v:
Physical Review B 105(2022), 144103
Physical Review B
Physical Review B, 2022, 105, ⟨10.1103/PhysRevB.105.144103⟩
Physical Review B
Physical Review B, 2022, 105, ⟨10.1103/PhysRevB.105.144103⟩
International audience; The martensitic transformation is a fundamental physical phenomenon at the origin of important industrial applications. However, the underlying microscopic mechanism, which is of critical importance to explain the outstanding
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::80b25ec47ca349f513c9491228438343
https://www.hzdr.de/publications/Publ-35474-1
https://www.hzdr.de/publications/Publ-35474-1
Publikováno v:
The American Mineralogist
The American Mineralogist, 2016, 101 (7), pp.1560-1570. ⟨10.2138/am-2016-5561⟩
American Mineralogist
American Mineralogist, Mineralogical Society of America, 2016, 101 (7), pp.1560-1570. ⟨10.2138/am-2016-5561⟩
The American Mineralogist, 2016, 101 (7), pp.1560-1570. ⟨10.2138/am-2016-5561⟩
American Mineralogist
American Mineralogist, Mineralogical Society of America, 2016, 101 (7), pp.1560-1570. ⟨10.2138/am-2016-5561⟩
Using large volume press, samples of bridgmanites (Bg) in equilibrium with both silicate melt and liquid Fe-alloy were synthesized to replicate the early period of core-mantle segregation and magma ocean crystallization. We observe that the Fe partit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::46aeb7c03f8a04908208b6398158c819
https://uca.hal.science/hal-01637061
https://uca.hal.science/hal-01637061
Autor:
Denis Andrault, Nathalie Bolfan-Casanova, Steeve Gréaux, M. Ali Bouhifd, Nicolas Guignot, Laurent Gautron
Publikováno v:
Physics of the Earth and Planetary Interiors
Physics of the Earth and Planetary Interiors, Elsevier, 2009, 174, pp.254-263. ⟨10.1016/j.pepi.2008.06.010⟩
Physics of the Earth and Planetary Interiors, 2009, 174, pp.254-263. ⟨10.1016/j.pepi.2008.06.010⟩
Physics of the Earth and Planetary Interiors, Elsevier, 2009, 174, pp.254-263. ⟨10.1016/j.pepi.2008.06.010⟩
Physics of the Earth and Planetary Interiors, 2009, 174, pp.254-263. ⟨10.1016/j.pepi.2008.06.010⟩
The high ability of the Al-rich CaSiO 3 perovskite to contain large amounts of uranium (up to 4 at.% U) has been studied up to 54 GPa and 2400 K, using laser-heated diamond anvil cell (LH-DAC) and up to 18 GPa and 2200 K using a multi-anvil press (MA
Publikováno v:
American Mineralogist. 94:1-16
We used configurational entropy theory to model the viscosity (η) of hydrous melts of NaAlSi 3 O 8 , haplogranite (SiO 2 -KAlSi 3 O 8 -NaAlSi 3 O 8 ), and complex (natural) granite composition from available measurements and recently published confi
Autor:
Andrew P. Jephcoat, M. Ali Bouhifd
Publikováno v:
Nature. 439:961-964
Understanding of the crystal chemistry of the Earth's deep mantle has evolved rapidly recently with the gradual acceptance of the importance of the effect of minor elements such as aluminium on the properties of major phases such as perovskite1,2,3.
Publikováno v:
Earth and Planetary Science Letters. 218:31-44
As measured in air above the glass transition range, the viscosity of an alkali basalt increases markedly with time by about two orders of magnitude in 12 h. This effect is essentially physical and due to the presence of microcrystals although partia