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dc.contributor.advisorPignotta, Geoffrey S.
dc.contributor.authorSchwierske, Kelly L.
dc.date.accessioned2015-02-09T19:51:30Z
dc.date.available2015-02-09T19:51:30Z
dc.date.issued2014-04
dc.identifier.urihttp://digital.library.wisc.edu/1793/70483
dc.descriptionColor poster with text, maps, images, and graphs.en
dc.description.abstractThe Gafvert Lake sequence comprises part of the Vermilion District in the Wawa-Abitibi Terrane in northeastern Minnesota and is located in Minnesota's newest state park, Lake Vermilion State Park. The Neoachean Gafvert Lake sequence is a 2.7 billion year old volcanic and plutonic complex similar to those found in modern subduction zone settings. The purpose of this study was to provide a better understanding of the geological, volcanological, geochemical, tectonic and mineralization processes, as well as age relationships associated with its development.en
dc.description.sponsorshipUniversity of Wisconsin--Eau Claire Office of Research and Sponsored Programs.en
dc.language.isoen_USen
dc.relation.ispartofseriesUSGZE AS589en
dc.subjectGafvert Lake Sequence (Minn.)en
dc.subjectLake Vermilion State Park (Minn.)en
dc.subjectGeologyen
dc.subjectGeochemistryen
dc.subjectPostersen
dc.title2.7 Billion Year Old Mt. St. Helens of Northern Minnesota : Petrography and Geochemistry of the Neoarchean Gafvert Lake Sequenceen
dc.typePresentationen


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