Zobrazeno 1 - 8
of 8
pro vyhledávání: '"N. J. DiFrancesco"'
Autor:
Marina Gemma, Dante S. Lauretta, K. T. Howard, G. Kim, N. J. DiFrancesco, Hanna Nekvasil, A. D. Rogers, Alexander Kling, Timothy D. Glotch, V. E. Hamilton, P. R. Christensen, L. B. Breitenfeld, Denton S. Ebel
Publikováno v:
Journal of Geophysical Research: Planets. 126
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c155f7cb619cead3bb9b7dfe94b85b04
https://doi.org/10.1029/2021je007035
https://doi.org/10.1029/2021je007035
Publikováno v:
Journal of Geophysical Research: Planets. 124:1592-1617
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e99d1ad93c9bd8783c2ed2e9b2d028ad
https://doi.org/10.1029/2018je005911
https://doi.org/10.1029/2018je005911
Publikováno v:
Journal of Geophysical Research: Planets. 123:1701-1722
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6bd97ab733d5e0cdc83fd5d6b2e0ac26
https://doi.org/10.1029/2018je005523
https://doi.org/10.1029/2018je005523
Autor:
N. J. DiFrancesco, Hanna Nekvasil
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ad1256afdadda374c3858903bf9f0bcc
https://doi.org/10.1130/abs/2019am-338722
https://doi.org/10.1130/abs/2019am-338722
Publikováno v:
American Mineralogist. 100:983-990
The presence of anorthosite in the lunar highlands containing plagioclase that is compositionally less calcic than plagioclase in the ferroan anorthosites cannot be readily explained by the current lunar paradigm in which lunar anorthosite was produc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::84a83332fb36523f03838c856841b543
https://doi.org/10.2138/am-2015-4885
https://doi.org/10.2138/am-2015-4885
Autor:
Oliver Lockwood, Douglas R. Schaub, N. J. DiFrancesco, Tristan Catalano, Donald H. Lindsley, Hanna Nekvasil
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::120aea66d538184f95bbe16ae1b7aa43
https://doi.org/10.1130/abs/2017am-305312
https://doi.org/10.1130/abs/2017am-305312
Publikováno v:
Journal of Petrology. 48:365-393
Basaltic magmas found in intraplate suites appear to follow more than one differentiation trend. Many ocean island suites follow the ocean island tholeiitic trend, with the basalts differentiating from olivine tholeiite through basaltic andesite, and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6829a2b1db8f1199d30a23ea4e20732b
https://doi.org/10.1093/petrology/egl063
https://doi.org/10.1093/petrology/egl063
Publikováno v:
Journal of Petrology; Feb2007, Vol. 48 Issue 2, p365-365, 1p