John C. Behrendt
University of Colorado (also USGS Boulder), Boulder, CO
Activity
2016
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GLIMPCE SEISMIC REFLECTION EVIDENCE OF DEEP-CRUSTAL AND UPPER MANTLE INTRUSIONS AND MAGMATIC UNDERPLATING ASSOCIATED WITH THE MIDCONTINENT RIFT SYSTEM (MRS) OF NORTH AMERICA – ANOTHER LOOK
T7 Precambrian Evolution and Mineral Resources of the Midcontinent Rift Region I: In Honor of William J. HinzeSunday, 25 September 20168:00 AM - 12:00 PMRoom 407
2013
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VOLCANIC ROCKS AND SUBGLACIAL VOLCANISM BENEATH THE WEST ANTARCTIC ICE SHEET (WAIS) IN THE WEST ANTARCTIC RIFT SYSTEM, FROM AEROMAGNETIC AND RADAR ICE SOUNDING - THIEL SUBGLACIAL VOLCANO AS POSSIBLE SOURCE OF THE ASH LAYER IN THE WAISCORE
T174 Combining Geophysics and Geology: The George P. Woollard Award SessionMonday, 28 October 20131:00 PM - 5:00 PMRoom 402
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A HALF CENTURY OF ANTARCTIC GEOSCIENCE EXPLORATION, 1957-2013
2 125 Anniversary Pardee Symposium: 125 Years of Exploration and Geoscience with GSA and the National Geographic Society: Celebrating the Rich History of Geoscientist Explorers Who Have Broadened Our Horizons and Knowledge of Our WorldSunday, 27 October 20138:00 AM - 12:00 PMMile High Ballroom 4AB
2010
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ACTIVE-RECENT SUBGLACIAL VOLCANISM WITHIN THE WEST ANTARCTIC RIFT SYSTEM, INTERPRETED FROM AEROMAGNETIC AND RADAR ICE SOUNDING MAY EFFECT THE STABILITY OF THE WEST ANTARCTIC ICE SHEET (WAIS) WHICH FLOWS THROUGH IT
T98 Controls and Consequences of Continental Rifting: From Heat Flow, Stress, and Strain to Magmatism, Landscape-Basin Evolution, and Development of Natural ResourcesMonday, 1 November 20108:00 AM - 12:00 PMLobby F