An 57Fe Mössbauer study of three Australian L5 ordinary-chondrite meteorites: dating Kinclaven–001
| dc.contributor.author | Cadogan, J. | |
| dc.contributor.author | Rebbouh, L. | |
| dc.contributor.author | Mills, J. | |
| dc.contributor.author | Bland, Phil | |
| dc.date.accessioned | 2017-01-30T14:56:56Z | |
| dc.date.available | 2017-01-30T14:56:56Z | |
| dc.date.created | 2014-02-12T20:00:37Z | |
| dc.date.issued | 2013 | |
| dc.identifier.citation | Cadogan, J.M. and Rebbouh, L. and Mills, J.V.J. and Bland, P.A. 2013. An 57Fe Mössbauer study of three Australian L5 ordinary-chondrite meteorites: Dating Kinclaven–001. Hyperfine Interactions. 222 (S2): pp. 91-98. | |
| dc.identifier.uri | http://hdl.handle.net/20.500.11937/42036 | |
| dc.identifier.doi | 10.1007/s10751-012-0644-1 | |
| dc.description.abstract |
Three L5-type ordinary chondrite meteorites recovered from the Nullarbor Region of Western Australia were studied by 57Fe Mössbauer spectroscopy: Kinclaven–001, Camel Donga–007 and Gunnadorah–002. The relative amounts of the various Fe-bearing phases including the primary minerals (Olivine,Pyroxene, Troilite and Fe-Ni metal) and the ferric alteration products (Goethite, Maghemite/Magnetite) were obtained to determine the percentage of iron converted to Fe3+ by weathering processes. These data allow us to estimate the terrestrial age of Kinclaven–001 at 1,700 ± 1,300 yrs. | |
| dc.publisher | Kluwer Academic Publishers | |
| dc.subject | Meteorites · Mössbauer | |
| dc.title | An 57Fe Mössbauer study of three Australian L5 ordinary-chondrite meteorites: dating Kinclaven–001 | |
| dc.type | Journal Article | |
| dcterms.source.volume | 222 | |
| dcterms.source.startPage | 91 | |
| dcterms.source.endPage | 98 | |
| dcterms.source.issn | 03043843 | |
| dcterms.source.title | Hyperfine Interactions | |
| curtin.department | ||
| curtin.accessStatus | Fulltext not available |