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Graphite-Based Geothermometry on Almahata Sitta Ureilitic Meteorites

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dc.contributor.author Barbaro, Anna
dc.contributor.author Domeneghetti, M. Chiara
dc.contributor.author Goodrich, Cyrena Anne
dc.contributor.author Meneghetti, Moreno
dc.contributor.author Litti, Lucio
dc.contributor.author Fioretti, Anna Maria
dc.contributor.author Jenniskens, Petrus Matheus Marie
dc.contributor.author Shaddad, Muawia H.
dc.contributor.author Nestola, Fabrizio
dc.date.accessioned 2020-11-13T21:06:10Z
dc.date.available 2020-11-13T21:06:10Z
dc.date.issued 2020-11-12
dc.identifier.citation Barbaro, A.; Domeneghetti, M.C.; Goodrich, C.A.; Meneghetti, M.; Litti, L.; Fioretti, A.M.; Jenniskens, P.; Shaddad, M.H.; Nestola, F. Graphite-Based Geothermometry on Almahata Sitta Ureilitic Meteorites. Minerals 2020, 10, 1005. en
dc.identifier.other DOI:10.3390/min10111005
dc.identifier.uri https://hdl.handle.net/20.500.11753/1724
dc.description.abstract The thermal history of carbon phases, including graphite and diamond, in the ureilite meteorites has implications for the formation, igneous evolution, and impact disruption of their parent body early in the history of the Solar System. Geothermometry data were obtained by micro-Raman spectroscopy on graphite in Almahata Sitta (AhS) ureilites AhS 72, AhS 209b and AhS A135A from the University of Khartoum collection. en
dc.format.extent 14 pages
dc.format.mimetype application/pdf
dc.language.iso en en
dc.publisher MDPI en
dc.relation.ispartofseries LPI contribution ; no. 2569
dc.subject Meteorites en
dc.subject Graphite en
dc.title Graphite-Based Geothermometry on Almahata Sitta Ureilitic Meteorites en
dc.type Article en
dc.rights.license This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited


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