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 (Dataset)

Matthew A. Coble; Gail A. Mahood;

2016 || Magnetics Information Consortium (MagIC)

Paleomagnetic, rock magnetic, or geomagnetic data found in the MagIC data repository from a paper titled: Matthew A. Coble, Gail A. Mahood (2016). 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. Geosphere 12 (1):58-113. doi:10.1130/ges01162.1.

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Source http://dx.doi.org/10.7288/V4/MAGIC/16263
Source publisher Magnetics Information Consortium (MagIC)
DOI 10.7288/V4/MAGIC/16263
Authors
  • Matthew A. Coble
  • Gail A. Mahood
Contributors
  • Magnetics Information Consortium (MagIC)
  • Distributor
References
  • Coble, M. A., & Mahood, G. A. (2015). 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. Geosphere, 12(1), 58–113. https://doi.org/10.1130/ges01162.1
  • 10.1130/GES01162.1
  • IsDocumentedBy
Citation Coble, M. A., & Mahood, G. A. (2016). 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 (Dataset) (Version 6) [Data set]. Geosphere. https://doi.org/10.7288/V4/MAGIC/16263