James D. Kirkpatrick
McGill University, Montreal, QC
Activity
2015
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WEAR AND RE-ROUGHENING PROCESSES IN A SINGLE FAULT ZONE CHARACTERIZED BY STRUCTURE FROM MOTION
T318 Strike Slip Fault Systems Transfer Stress Inboard from the Subduction Zone Margin Leading to Basin Subsidence and Orogensis, Are Conduits for Magmatism, and Are Responsible for Far-Traveled Terrane Translation (Posters)Wednesday, 4 November 20159:00 AM - 6:30 PMExhibit Hall
2014
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STRUCTURE OF THE PLATE BOUNDARY FAULT IN THE JAPAN TRENCH, AND IMPLICATIONS FOR SLIP BEHAVIOUR
T91 Deformation Localization throughout the CrustMonday, 20 October 20148:00 AM - 12:00 PM118
2013
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TRANSITIONAL DUCTILE TO BRITTLE STRIKE-SLIP RHEOLOGY: AN EXHUMED LABORATORY OF THE SEISMOGENIC ZONE IN THE EASTERN CENTRAL SIERRA NEVADA, CALIFORNIA
T371 The Rock Record of Fault Rheology and Slip Dynamics (Posters)Wednesday, 30 October 20139:00 AM - 6:30 PMHall D
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SILICA LUBRICATION IN FAULTS
T326 Structure and Evolution of Brittle Faults and Fault Rocks: Physical Properties, Geometry, and Geochemical Changes that Influence Water, Energy, and Mineral ResourcesWednesday, 30 October 20138:00 AM - 12:00 PMRoom 507
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SCALE DEPENDENT INFLUENCE OF PRE-EXISTING SHEAR ZONES ON BRITTLE FAULT GEOMETRY, ARCHITECTURE AND FLUID FLOW STRUCTURE DURING RIFTING
T217 The Role of Tectonic Inheritance in Continental ExtensionTuesday, 29 October 20138:00 AM - 12:00 PMRoom 507