A previously unrecognized example of the shock-induced breakdown of biotite to garnet from the Steen River impact structure, Canada

dc.contributor.authorWalton, Erin L.
dc.contributor.authorSharp, Thomas
dc.contributor.authorHu, Jinping
dc.contributor.authorTschauner, Oliver
dc.date.accessioned2016-10-07
dc.date.accessioned2022-05-28T00:36:23Z
dc.date.available2022-05-28T00:36:23Z
dc.date.issued2016
dc.descriptionPresented on August 7-12, 2016 at the Annual Meeting of the Meteoritical Society held at the Henry Ford Building in Berlin, Germany.
dc.description.abstractShock metamorphic effects from quartz and feldspar have been studied in detail, and to a lesser extent olivine and pyroxene. Less is known about how shock is manifest in other minerals such as double chain inosilicates, phyllosilicates, carbonates and sulfates. In this study, we investigate shock in crystalline basement rocks from the Steen River impact structure (SRIS), a 25-km diameter complex crater in NW Alberta, Canada.
dc.format.extent95.48 KB
dc.format.mimetypePDF
dc.identifier.urihttps://hdl.handle.net/20.500.14078/600
dc.languageEnglish
dc.language.isoen
dc.rightsAll Rights Reserved
dc.subjectshock
dc.subjectcrystalline basement rocks
dc.subjectimpact structures
dc.titleA previously unrecognized example of the shock-induced breakdown of biotite to garnet from the Steen River impact structure, Canada
dc.typePresentation
dspace.entity.type
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