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- W2743758317 startingPage "1066" @default.
- W2743758317 abstract "The McDermitt caldera (western USA) is commonly considered the point of origin of the Yellowstone hotspot, yet until now no geologic map existed of the caldera and its geology and development were incompletely documented. We developed a comprehensive geologic framework through detailed and reconnaissance geologic mapping, extensive petrographic and chemical analysis, and high-precision 40Ar/39Ar dating. The caldera formed during eruption of the 16.39 ± 0.02 Ma (n = 3) McDermitt Tuff (named here), which is strongly zoned from peralkaline, aphyric, high-Si rhyolite (comendite) to metaluminous, abundantly anorthoclase-phyric, trachydacite, or Fe-rich andesite (icelandite)." @default.
- W2743758317 created "2017-08-17" @default.
- W2743758317 creator A5031043985 @default.
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- W2743758317 date "2017-07-17" @default.
- W2743758317 modified "2023-10-16" @default.
- W2743758317 title "Geology and evolution of the McDermitt caldera, northern Nevada and southeastern Oregon, western USA" @default.
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- W2743758317 doi "https://doi.org/10.1130/ges01454.1" @default.
- W2743758317 hasPublicationYear "2017" @default.
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