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dc.contributor.authorHumayun, M.
dc.contributor.authorNemchin, Alexander
dc.contributor.authorGrange, M.
dc.contributor.authorKennedy, A.
dc.contributor.authorZanda, B.
dc.contributor.authorHewins, R.
dc.contributor.authorLorand, J.
dc.contributor.authorGoepel, C.
dc.contributor.authorLewin, E.
dc.contributor.authorPont, S.
dc.contributor.authorDeldicque, D.
dc.date.accessioned2017-01-30T11:52:37Z
dc.date.available2017-01-30T11:52:37Z
dc.date.created2015-10-29T04:09:32Z
dc.date.issued2013
dc.identifier.citationHumayun, M. and Nemchin, A. and Grange, M. and Kennedy, A. and Zanda, B. and Hewins, R. and Lorand, J. et al. 2013. The Age and Composition of the Martian Crust from NWA 7533, in Proceedings of the 76th Annual Meeting of the Meteoritical-Society, Jul 29-Aug 7 2013, id 5198. Edmonton, Canada: Lunar and Planetary Institute.
dc.identifier.urihttp://hdl.handle.net/20.500.11937/15906
dc.description.abstract

NWA 7533 is a pre-Noachian regolith breccia, containing siderophiles consistent with 5% chondritic impactor, 4.44 Ga zircons, and LILE enrichments implying a crustal thickness of 50 km established in the first 100 Ma of martian history.

dc.publisherWILEY-BLACKWELL
dc.relation.urihttp://www.hou.usra.edu/meetings/metsoc2013/pdf/5198.pdf
dc.titleThe Age and Composition of the Martian Crust from NWA 7533
dc.typeConference Paper
dcterms.source.volume48
dcterms.source.startPageA177
dcterms.source.endPageA177
dcterms.source.issn1086-9379
dcterms.source.seriesMETEORITICS & PLANETARY SCIENCE
dcterms.source.conference76th Annual Meeting of the Meteoritical-Society
curtin.departmentDepartment of Applied Geology
curtin.accessStatusFulltext not available


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