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dc.contributor.advisorIhinger, Phillip D.
dc.contributor.authorConde, Giselle
dc.date.accessioned2009-07-22T15:18:43Z
dc.date.available2009-07-22T15:18:43Z
dc.date.issued2009-07-22T15:18:43Z
dc.identifier.urihttp://digital.library.wisc.edu/1793/35578
dc.descriptionColor poster with text, images, maps, and graphs (Spring 2009)en
dc.description.abstractSupervolcano eruptions represent some of the most dramatic events in the geologic history of our planet. They form as a result of volatile exsolution from a viscous silica-rich melt structure. As water is the dominant volatile released in these eruptions, it is essential that we understand the solubility and speciation of water in felsic melt. This study provides micro-FTIR analyses on a suite of 30 obsidian flows from Anatolia.en
dc.description.sponsorshipUniversity of Wisconsin--Eau Claire Office of Research and Sponsored Programs.en
dc.language.isoen_USen
dc.relation.ispartofseriesUSGZE AS589en
dc.subjectSupervolcanoes--Turkeyen
dc.subjectVolcanic ash, tuff, etc.--Researchen
dc.subjectObsidian--Inclusionsen
dc.subjectPostersen
dc.subjectHydration rind datingen
dc.titleWater Speciation in Anatolian Obsidian : Quenched Magmatic Water vs. Low Temperature Hydrationen
dc.title.alternativeWater Speciation in Natural Obsidian : Two Thermal Regimes of Hydrationen
dc.typePresentationen


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