Please use this identifier to cite or link to this item: http://hdl.handle.net/1893/17073
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dc.contributor.authorMcSween, Harry Y-
dc.contributor.authorWyatt, Michael B-
dc.contributor.authorGellert, Ralf-
dc.contributor.authorBell, III James F-
dc.contributor.authorMorris, Richard Van-
dc.contributor.authorHerkenhoff, Kenneth E-
dc.contributor.authorCrumpler, Larry S-
dc.contributor.authorMilam, Keith A-
dc.contributor.authorStockstill, Karen R-
dc.contributor.authorTornabene, Livio L-
dc.contributor.authorArvidson, Raymond E-
dc.contributor.authorBartlett, Paul W-
dc.contributor.authorBlaney, Diana-
dc.contributor.authorCabrol, Nathalie A-
dc.contributor.authorSchröder, Christian-
dc.date.accessioned2013-10-26T23:07:08Z-
dc.date.available2013-10-26T23:07:08Z-
dc.date.issued2006-01-06-
dc.identifier.otherS10-
dc.identifier.urihttp://hdl.handle.net/1893/17073-
dc.description.abstractRocks on the floor of Gusev crater are basalts of uniform composition and mineralogy. Olivine, the only mineral to have been identified or inferred from data by all instruments on the Spirit rover, is especially abundant in these rocks. These picritic basalts are similar in many respects to certain Martian meteorites (olivine-phyric shergottites). The olivine megacrysts in both have intermediate compositions, with modal abundances ranging up to 20–30%. Associated minerals in both include low-calcium and highcalcium pyroxenes, plagioclase of intermediate composition, iron-titanium-chromium oxides, and phosphate. These rocks also share minor element trends, reflected in their nickel-magnesium and chromium-magnesium ratios. Gusev basalts and shergottites appear to have formed from primitive magmas produced by melting an undepleted mantle at depth and erupted without significant fractionation. However, apparent differences between Gusev rocks and shergottites in their ages, plagioclase abundances, and volatile contents preclude direct correlation. Orbital determinations of global olivine distribution and compositions by thermal emission spectroscopy suggest that olivine-rich rocks may be widespread. Because weathering under acidic conditions preferentially attacks olivine and disguises such rocks beneath alteration rinds, picritic basalts formed from primitive magmas may even be a common component of the Martian crust formed during ancient and recent times.en_UK
dc.language.isoen-
dc.publisherWiley-Blackwell for the American Geophysical Union-
dc.relationMcSween HY, Wyatt MB, Gellert R, Bell III JF, Morris RV, Herkenhoff KE, Crumpler LS, Milam KA, Stockstill KR, Tornabene LL, Arvidson RE, Bartlett PW, Blaney D, Cabrol NA & Schröder C (2006) Characterization and petrologic interpretation of olivine-rich basalts at Gusev Crater, Mars, Journal of Geophysical Research: Planets, 111 (E2), Art. No.: S10.-
dc.rightsCopyright 2006 by the American Geophysical Union. AGU allows authors to deposit their journal articles if the version is the final published citable version of record, the AGU copyright statement is clearly visible on the posting, and the posting is made 6 months after official publication by the AGU.-
dc.subjectbasalten_UK
dc.subjectMarsen_UK
dc.subjectolivineen_UK
dc.titleCharacterization and petrologic interpretation of olivine-rich basalts at Gusev Crater, Marsen_UK
dc.typeJournal Articleen_UK
dc.identifier.doihttp://dx.doi.org/10.1029/2005JE002477-
dc.citation.jtitleJournal of Geophysical Research: Planets-
dc.citation.issn2169-9097-
dc.citation.volume111-
dc.citation.issueE2-
dc.citation.publicationstatusPublished-
dc.citation.peerreviewedRefereed-
dc.type.statusPublisher version (final published refereed version)-
dc.author.emailchristian.schroeder@stir.ac.uk-
dc.description.notesAdditional co-authors: PR Christensen, BC Clark, JA Crisp, DJ DesMarais, T Economou, JD Farmer, W Farrand, A Ghosh, M Golombek, S Gorevan, R Greeley, VE Hamilton, JR Johnson, BL Joliff, G Klingelhöfer, AT Knudson, S McLennan, D Ming, JE Moersch, R Rieder, SW Ruff, PA de Souza Jr, SW Squyres, H Wnke, A Wang, A Yen, J Zipfelen_UK
dc.contributor.affiliationUniversity of Tennessee-
dc.contributor.affiliationArizona State University-
dc.contributor.affiliationUniversity of Guelph-
dc.contributor.affiliationCornell University-
dc.contributor.affiliationNational Aeronautics and Space Administration (NASA)-
dc.contributor.affiliationU.S. Geological Survey-
dc.contributor.affiliationNew Mexico Museum of Natural History and Science-
dc.contributor.affiliationUniversity of Tennessee-
dc.contributor.affiliationUniversity of Tennessee-
dc.contributor.affiliationUniversity of Tennessee-
dc.contributor.affiliationWashington University In Saint Louis-
dc.contributor.affiliationHoneybee Robotics-
dc.contributor.affiliationCalifornia Institute of Technology-
dc.contributor.affiliationNational Aeronautics and Space Administration (NASA)-
dc.contributor.affiliationBiological and Environmental Sciences-
dc.identifier.isi000234510100003-
Appears in Collections:Biological and Environmental Sciences Journal Articles

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