Supplemental material: Geology of the High Rock caldera complex, northwest Nevada, and implications for intense rhyolitic volcanism associated with flood basalt magmatism and the initiation of the Snake River Plain–Yellowstone trend

Coble, Matthew A.; Mahood, Gail A.

doi:10.1130/GES01162.S4

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Supplemental material: Geology of the High Rock caldera complex, northwest Nevada, and implications for intense rhyolitic volcanism associated with flood basalt magmatism and the initiation of the Snake River Plain–Yellowstone trend

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posted on 2015-12-23, 00:00 authored by Matthew A. Coble, Gail A. Mahood

Geosphere, February 2016, v. 12, p. 58-113, doi:10.1130/GES01162.1, Supplemental Figure 1 - Isopach maps for ignimbrites in the High Rock caldera complex.

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Supplemental material: Geology of the High Rock caldera complex, northwest Nevada, and implications for intense rhyolitic volcanism associated with flood basalt magmatism and the initiation of the Snake River Plain–Yellowstone trend

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