J. Patchett
University of Arizona, Tucson, AZ
Activity
2013
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ISOTOPIC EVIDENCE FOR A LACUSTRINE ORIGIN FOR THE PLIOCENE BOUSE FORMATION IN THE LOWER COLORADO RIVER VALLEY
97 Special Session: CRevolution 2: Cenozoic Landscape Evolution of the Colorado Plateau–Rocky Mountain Region and the Carving of Grand Canyon IMonday, 28 October 20138:00 AM - 12:00 PMMile High Ballroom 4CD
2011
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ORIGIN AND EVOLUTION OF GRANITES IN THE SANTA CATALINA CORE COMPLEX, ARIZONA
243 Geochemistry (Posters)Wednesday, 12 October 20119:00 AM - 6:00 PMHall C
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CIRCA 4.8 MA AGE FOR INCEPTION OF THE MODERN COLORADO RIVER
T189 Limnogeology: Interdisciplinary Studies of Lakes and Paleolakes (Posters)Tuesday, 11 October 20119:00 AM - 6:00 PMHall C
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WHAT'S IN A NAME: EXTINCTIONS, EXCURSIONS, EVENTS AND EPIBOLES (OR WAS THIS HYPERBOLE?)
T14 Multidisciplinary Approaches to Studying the Causes and Consequences of Mass Extinction: Geochemistry, Paleoecology, and Paleoenvironments ISunday, 9 October 20118:00 AM - 12:00 PMRoom 200H-J
2007
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JURASSIC TO EOCENE MAGMATIC HISTORY OF THE COAST MOUNTAINS BATHOLITH IN NORTH-COASTAL BRITISH COLUMBIA
T196 Geochemistry of Magmatic and Metamorphic Processes I: In Honor of the Contributions of Joseph L. WoodenWednesday, 31 October 20078:00 AM - 12:00 PM
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A LATE MIOCENE-EARLY PLIOCENE CHAIN OF LAKES FED BY THE COLORADO RIVER: EVIDENCE FROM SR ISOTOPES OF THE BOUSE FORMATION BETWEEN GRAND CANYON AND THE GULF OF CALIFORNIA
T160 Inland Waters, Playas and Saline Lakes: More than Mini-OceansTuesday, 30 October 20071:30 PM - 5:30 PM