Please use this identifier to cite or link to this item: https://hdl.handle.net/10593/3338
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dc.contributor.authorOwocki, Krzysztof-
dc.contributor.authorMuszyński, Andrzej-
dc.date.accessioned2012-09-12T07:50:10Z-
dc.date.available2012-09-12T07:50:10Z-
dc.date.issued2012-09-12T07:50:10Z-
dc.identifier.issn1426-8981-
dc.identifier.urihttp://hdl.handle.net/10593/3338-
dc.description.abstractA specimen of the Sahara 02500 ordinary chondrite contains shock-produced veins consisting of recrystallised fine- grained pyroxenes that include small droplets of Ni-rich metal. Non-melted olivines and pyroxenes show planar deformations filled by shock-melted and -polluted metal and troilite. Shock-melted feldspathic glass is present close to the shock veins. Geothermometric estimations indicate that the meteorite locally experienced moderate shock metamorphism with a minimum local peak temperature above 1400ºC, resulting in partial melting of Ca-poor pyroxene and full melting of feldspars, metal and sulphides. The mineral assemblage in the shock veins suggests a pressure during melt recrystallisation below 10 GPa.pl_PL
dc.language.isoenpl_PL
dc.publisherWydawnictwo Naukowe UAM
dc.relation.ispartofseries18, (2);111-118-
dc.subjectOrdinary chondritepl_PL
dc.subjectShock veinspl_PL
dc.subjectSubsolidus recrystallizationpl_PL
dc.titleShock veins in the Sahara 02500 ordinary chondritepl_PL
dc.typeArtykułpl_PL
Appears in Collections:Geologos, 2012, 18, 2

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