Diagenetic Patterns in Cambrian Sandstone in Western Wisconsin : Constraining Potential Sources of Airborne Particulate Matter

dc.contributor.advisorPignotta, Geoffrey S.
dc.contributor.advisorSyverson, Kent M.
dc.contributor.authorPoirer, Justin M.
dc.contributor.authorFlifet, Rachel
dc.contributor.authorBlotz, Kaelyn E.
dc.date.accessioned2016-04-12T16:18:27Z
dc.date.available2016-04-12T16:18:27Z
dc.date.issued2015-04
dc.descriptionColor poster with text, maps, charts, and photographs.en
dc.description.abstractThe Wonewoc and Jordan formations of western Wisconsin are important sources of frac sand used in hydraulic fracturing. These units are valued by industry due to the ultra-pure composition, loosely consolidated nature and resistance to fracturing. Statistical analysis of raw and processed sand was undertaken to assess if grain fragmentation, as evidenced by fresh, conchoidal fracture faces, occurs during processing.en
dc.description.sponsorshipUniversity of Wisconsin--Eau Claire Office of Research and Sponsored Programsen
dc.identifier.urihttp://digital.library.wisc.edu/1793/74725
dc.language.isoen_USen
dc.relation.ispartofseriesUSGZE AS589en
dc.subjectCambrian sandstoneen
dc.subjectHydraulic fracturingen
dc.subjectFrac sand miningen
dc.subjectSilicaen
dc.subjectPostersen
dc.titleDiagenetic Patterns in Cambrian Sandstone in Western Wisconsin : Constraining Potential Sources of Airborne Particulate Matteren
dc.typePresentationen

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