A. Mulch
Univ of Minnesota, Minneapolis, MN
Activity
2005
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THE ROLE OF FAULTS IN ISOTOPE TRANSPORT AND EXCHANGE DURING THE FORMATION OF THE SHUSWAP METAMORPHIC CORE COMPLEX, BRITISH COLUMBIA
T106 Fault Zone Controls on Fluid Movement, Earth Resources and Processes: Perspectives from Field, Laboratory, and Modeling Studies IIMonday, 17 October 20051:30 PM - 5:30 PM
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TOPOGRAPHY OF THE EOCENE SIERRA NEVADA: EVIDENCE FROM STABLE ISOTOPES OF KAOLINITE IN PALEO-STREAM CHANNELS
37 Provenance and Tectonics: New Models and Recent AdvancesSunday, 1 May 20058:20 AM - 12:00 PM
2004
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FLUID FLOW AND HEAT TRANSFER DURING EXHUMATION OF METAMORPHIC CORE COMPLEXES
T237 Low-angle Normal Faults and Faulting: Field Studies, Fault Rocks, Mechanics, and Weakening MechanismsWednesday, 10 November 20041:30 PM - 5:30 PM
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TIME SCALES OF FLUID FLOW AND THERMAL RELAXATION DURING HIGH-STRESS DEFORMATION IN EXTENSIONAL DETACHMENT MYLONITE
T237 Low-angle Normal Faults and Faulting: Field Studies, Fault Rocks, Mechanics, and Weakening MechanismsWednesday, 10 November 20041:30 PM - 5:30 PM
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HOW HIGH WAS THE CORDILLERA? EOCENE ELEVATION OF THE NORTH AMERICAN CORDILLERA RECORDED IN STABLE ISOTOPE COMPOSITION OF DETACHMENT MYLONITES
T42 Pre-EarthScope Synthesis of the Rocky Mountains I and II: Surface Processes, Geodynamics, and the Roles of Neotectonics and Climate in Development of Modern TopographySunday, 7 November 20041:30 PM - 5:30 PM