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dc.contributor.authorOsinski, Gordon R.
dc.date.accessioned2021-02-12T20:56:26Z
dc.date.available2021-02-12T20:56:26Z
dc.date.issued2003-01-01
dc.identifier.citationOsinski, G. R. (2003). Impact glasses in fallout suevites from the Ries impact structure, Germany: An analytical SEM study. Meteoritics & Planetary Science, 38(11), 1641-1667.
dc.identifier.issn1945-5100
dc.identifier.doi10.1111/j.1945-5100.2003.tb00006.x
dc.identifier.urihttp://hdl.handle.net/10150/655766
dc.description.abstractImpact-generated glasses from fallout suevite deposits at the Ries impact structure have been investigated using analytical scanning electron microscopy. Approximately 320 analyses of glass clasts were obtained. Four glass types are distinguished on the basis of composition and microtextures. Type 1 glasses correspond to the aerodynamically shaped glass bombs studied previously by many workers. Major oxide concentrations indicate the involvement of granitic rocks, amphibolites, and minor Al-rich gneisses during melting. Type 2 glasses are chemically heterogeneous, even within individual clasts, with variations of several wt% in most of the major oxides (e.g., 57-70 wt% SiO2). This suggests incomplete mixing of: 1) mineral-derived melts or 2) whole rock melts from a wide range of lithologies. Aluminium-rich clinopyroxene and Fe-Mg-rich plagioclase quench crystals are present in type 1 and 2 glasses, respectively. Type 3 glasses contain substantial amounts of H2O (~12-17 wt%), low SiO2 (50-53 wt%), high Al2O3 (17-21 wt%), and high CaO (57 wt%) contents. This suggests an origin due to shock melting of part of the sedimentary cover. Type 4 glasses form a ubiquitous component of the suevites. Based on their high SiO2 content (~85-100 wt%), the only possible protolith are sandstones in the lowermost part of the sedimentary succession. Calcite forms globules within type 1 glasses, with which it develops microtextures indicative of liquid immiscibility. Unequivocal evidence also exists for liquid immiscibility between what are now montmorillonite globules and type 1, 2, and 4 glasses, indicating that montmorillonite was originally an impact melt glass. Clearly, the melt zone at the Ries must have incorporated a substantial fraction of the sedimentary cover, as well as the underlying crystalline basement rocks. Impact melts were derived from different target lithologies and these separate disaggregated melts did not substantially mix in most cases (type 2, 3, and 4 glasses and carbonate melts).
dc.language.isoen
dc.publisherThe Meteoritical Society
dc.relation.urlhttps://meteoritical.org/
dc.rightsCopyright © The Meteoritical Society
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/
dc.subjectQuench crystallization
dc.subjectCarbonate melts
dc.subjectimpact glasses
dc.titleImpact glasses in fallout suevites from the Ries impact structure, Germany: An analytical SEM study
dc.typeArticle
dc.typetext
dc.identifier.journalMeteoritics & Planetary Science
dc.description.collectioninformationThe Meteoritics & Planetary Science archives are made available by the Meteoritical Society and the University of Arizona Libraries. Contact lbry-journals@email.arizona.edu for further information.
dc.eprint.versionFinal published version
dc.description.admin-noteMigrated from OJS platform February 2021
dc.source.volume38
dc.source.issue11
dc.source.beginpage1641
dc.source.endpage1667
refterms.dateFOA2021-02-12T20:56:26Z


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