Diverse mid-Miocene silicic volcanism associated with the Yellowstone–Newberry thermal anomaly

@article{Brueseke2007DiverseMS,
  title={Diverse mid-Miocene silicic volcanism associated with the Yellowstone–Newberry thermal anomaly},
  author={M. E. Brueseke and W. Hart and M. Heizler},
  journal={Bulletin of Volcanology},
  year={2007},
  volume={70},
  pages={343-360}
}
  • M. E. Brueseke, W. Hart, M. Heizler
  • Published 2007
  • Geology
  • Bulletin of Volcanology
  • The Santa Rosa–Calico volcanic field (SC) of northern Nevada is a complex, multi-vent mid-Miocene eruptive complex that formed in response to regional lithospheric extension and flood basalt volcanism. Santa Rosa–Calico volcanism initiated at ∼16.7 Ma, concurrent with regional Steens–Columbia River flood basalt activity and is characterized by a complete compositional spectrum of basalt through high-silica rhyolite. To better understand the relationships between upwelling mafic magmatism… CONTINUE READING

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