Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Justin Y. Hu"'
Autor:
Jin Liu, Nicolas Dauphas, Mathieu Roskosz, Michael Y. Hu, Hong Yang, Wenli Bi, Jiyong Zhao, Esen E. Alp, Justin Y. Hu, Jung-Fu Lin
Publikováno v:
Nature Communications, Vol 8, Iss 1, Pp 1-6 (2017)
Terrestrial basalts have a unique iron isotopic signature taken as fingerprints of core formation. Here, high pressure studies show that force constants of iron bonds increase with pressure similarly for silicate and metals suggesting interplanetary
Externí odkaz:
https://doaj.org/article/2f4834cb57434e2698e38dcc342e26ce
Autor:
Justin Y. Hu, Nicolas Dauphas, Nicole X. Nie, Mathieu Roskosz, Xi Chen, Andy W. Heard, Zhe J. Zhang, Hao Zeng, Esen E. Alp, Michael Y. Hu, Jiyong Zhao
Publikováno v:
Geochimica et Cosmochimica Acta. 348:323-339
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a835d66fefb7301dd276c3988ce9f45d
https://doi.org/10.1016/j.gca.2023.03.002
https://doi.org/10.1016/j.gca.2023.03.002
Autor:
Andy W. Heard, Nicolas Dauphas, Isaac L. Hinz, Jena E. Johnson, Marc Blanchard, Esen E. Alp, Michael Y. Hu, Jiyong Zhao, Barbara Lavina, Mark E. Fornace, Justin Y. Hu, Mathieu Roskosz, Corliss Kin I Sio, Nicole X. Nie, Benoît Baptiste
Publikováno v:
ACS Earth and Space Chemistry
ACS Earth and Space Chemistry, 2023, ⟨10.1021/acsearthspacechem.2c00313⟩
ACS Earth and Space Chemistry, 2023, ⟨10.1021/acsearthspacechem.2c00313⟩
International audience; Iron formations (IFs) are chemical sedimentary rocks that were widely deposited before the Great Oxidation Event (GOE) around 2.4–2.2 Ga. It is generally thought that IFs precipitated as hydrated Fe3+ oxides (HFOs) such as f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::becaf91947d4360edbc2bee65e40bf03
https://doi.org/10.1021/acsearthspacechem.2c00313
https://doi.org/10.1021/acsearthspacechem.2c00313
Autor:
Nicolas Dauphas, Nicole X. Nie, Marc Blanchard, Zhe J. Zhang, Hao Zeng, Justin Y. Hu, Merlin Meheut, Channon Visscher, Robin Canup, Timo Hopp
Publikováno v:
The Planetary Science Journal
The Planetary Science Journal, 2022, 3, ⟨10.3847/PSJ/ac2e09⟩
The Planetary Science Journal, 2022, 3, ⟨10.3847/PSJ/ac2e09⟩
Moderately volatile elements (MVEs) are depleted and isotopically fractionated in the Moon relative to Earth. To understand how the composition of the Moon was established, we calculate the equilibrium and kinetic isotopic fractionation factors assoc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a37ba1c5b99dc471dbb9f816f45d96d4
https://hal-insu.archives-ouvertes.fr/insu-03661489/document
https://hal-insu.archives-ouvertes.fr/insu-03661489/document
