Petrography, Geochemistry, and Geochronology of the Green Mountain Shield Volcano, Oregon

dc.contributor.advisorCastonguay, Sammy R.
dc.contributor.authorFriedemann, Chase A.
dc.contributor.authorFriedrichs, Forest R.
dc.date.accessioned2016-03-22T16:57:26Z
dc.date.available2016-03-22T16:57:26Z
dc.date.issued2015-04
dc.descriptionColor poster with text, maps, and graphs.en
dc.description.abstractGreen Mountain (GM) is a small (~25km) shield volcano located in central Oregon. The ~740,000 year old shield, and associated young (~13,000 ya; Mackey et al., 2014) lava fields, are approximately ~50 km southeast of the Newberry Caldera on the northwest side of an age progressive trend of bi-model volcanism from southeastern Oregon to Newberry (Jordan, 2004). In a previous study(Friedrichs and Castonguay, 2014), XRF results were reported and interpreted as evidence of a single magma chamber that had undergone fractional crystallization and a significant magma recharge event before the most recent volcanism. This study aims to expand on this existing knowledge by applying geochronology, detailed petrographic analysis, and additional XRF analysis.en
dc.description.sponsorshipUniversity of Wisconsin--Eau Claire Office of Research and Sponsored Programs.en
dc.identifier.urihttp://digital.library.wisc.edu/1793/74348
dc.language.isoen_USen
dc.relation.ispartofseriesUSGZE AS589en
dc.subjectGreen Mountain Shield Volcano (Or.)en
dc.subjectPetrographyen
dc.subjectX-ray fluorescence (XRF)en
dc.subjectVolcanoesen
dc.subjectGeochemistryen
dc.subjectPostersen
dc.titlePetrography, Geochemistry, and Geochronology of the Green Mountain Shield Volcano, Oregonen
dc.typePresentationen

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