Myron G. Best
Brigham Young University, Provo, UT
Activity
2014
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CONSTRAINTS ON THE ORIGIN OF SUBDUCTION-RELATED IGNIMBRITE FLAREUPS FROM SOURCE VOLUME CALCULATIONS: THE SOUTHERN GREAT BASIN IGNIMBRITE PROVINCE
T149 Continental Arcs #2: Processes at Arc to Magma Reservoir-Scale and Connections from Magma Source to VolcanoMonday, 20 October 20141:00 PM - 5:00 PM121
2012
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EXPLORING THE CONNECTIONS BETWEEN VERY LARGE VOLUME IGNIMBRITES AND INTRACALDERA PLUTONS: INTRUSIONS RELATED TO THE OLIGOCENE WAH WAH SPRINGS TUFF, GREAT BASIN, USA
236 Volcanology (Posters)Wednesday, 7 November 20129:00 AM - 6:00 PMHall B
2011
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THE GREAT BASIN ALTIPLANO AND THE MYTH OF LARGE-MAGNITUDE REGIONAL EXTENSION DURING THE IGNIMBRITE FLAREUP
2 From Contraction to Extension: The Mesozoic to Cenozoic Tectonic Evolution of the Northern Great Basin IWednesday, 18 May 20118:00 AM - 12:00 PMWillow
2009
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THE GREAT BASIN ALTIPLANO DURING THE MIDDLE CENOZOIC IGNIMBRITE FLAREUP: INSIGHTS FROM VOLCANIC ROCKS
10 Magmatism from the Mesozoic to the Present in the Great Basin and Colorado Plateaus: A Tribute to the Career of Myron G. BestTuesday, 12 May 20098:00 AM - 12:00 PM
2002
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PETROLOGY AND EMPLACEMENT OF THE COTTONWOOD WASH TUFF
4 Volcanology and Mineral Resources of the Great Basin and the Colorado Plateau Transition ZoneTuesday, 7 May 20028:00 AM - 10:00 AM
2001
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ISOTOPE (ND-SR-PB-O) PROVINCIALITY REVEALED BY TERTIARY VOLCANIC ROCKS FROM THE INDIAN PEAK AND CENTRAL NEVADA CALDERA COMPLEXES OF THE SOUTHERN GREAT BASIN
129 Igneous Petrology IIWednesday, 7 November 20011:30 PM - 5:30 PM