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The Northwest Africa 10416 olivine-phyric Martian basalt: product of magma mixing, assimilation and alteration

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dc.contributor.authorHerd, Christopher D. K.
dc.contributor.authorWalton, Erin L.
dc.contributor.authorZiegler, Karen
dc.contributor.authorVaci, Zoltan
dc.contributor.authorAgee, Carl B.
dc.contributor.authorMuttik, Nele
dc.date.accessioned2016-10-07
dc.date.accessioned2022-05-28T00:36:23Z
dc.date.available2022-05-28T00:36:23Z
dc.date.issued2016
dc.descriptionPresented on March 21-25, 2016 at the 47th Lunar and Planetary Science Conference held at the Woodlands Waterway Marriott Hotel and Convention Center in The Woodlands, Texas.
dc.description.abstractThe Northwest Africa (NWA) 10416 olivine-phyric basalt is distinct from other Martian basalts in several ways, including in the record of pre-terrestrial alteration preserved within it. Here we report the details of the mineralogy, petrology and geochemistry of this intriguing specimen, which suggest that the history of the rock includes assimilation of previously altered igneous phases.
dc.format.extent977.99 KB
dc.format.mimetypePDF
dc.identifier.urihttps://hdl.handle.net/20.500.14078/603
dc.languageEnglish
dc.language.isoen
dc.rightsAll Rights Reserved
dc.subjectbasalt
dc.subjectMars
dc.subjectmeteorites
dc.titleThe Northwest Africa 10416 olivine-phyric Martian basalt: product of magma mixing, assimilation and alterationen
dc.typePresentation
dspace.entity.type

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