W. Ashley Griffith
University of Texas at Arlington, Arlington, TX
Activity
2016
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EFFECTS OF STRAIN RATE AND LOAD PATH ON SCALING ROCK MECHANICS EXPERIMENTS TO NATURAL FAULT DAMAGE ZONES
117 New Approaches and Results in Structural Geology and NeotectonicsMonday, 26 September 20161:30 PM - 5:30 PMRoom 203
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INSIGHTS INTO EARTHQUAKE RUPTURE AND RECOVERY FROM PALEOSEISMIC FAULTS
T25 Deconstructing Damage: Holistic Perspectives on the Spatiotemporal Evolution of Brittle Fault ZonesSunday, 25 September 20168:00 AM - 12:00 PMRoom 203
2015
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COMPARING FORWARD MODEL TECTONIC BOUNDARY CONDITIONS IN AN OBLIQUELY-CONVERGENT MARGIN: A CASE STUDY FROM THE SOUTHERN ANDES
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
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NATURE OF CRUSTAL DEFORMATION ARISING FROM OBLIQUE SUBDUCTION: STRAIN PARTITIONING, STRIKE-SLIP FAULTING AND SLIVER MOTION IN THE SOUTHERN ANDES
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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SANDSTONE INJECTITES RECORD PRE- AND SYN-FOLDING DEFORMATION AT SHEEP MOUNTAIN ANTICLINE, WYOMING
T197 Applications of Structural Geology and Geomechanics in the Petroleum IndustryTuesday, 21 October 20148:00 AM - 12:00 PM207
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THE NUCLEATION OF BEDDING PLANE THRUSTS ON GEOMETRICAL IRREGULARITIES: EVIDENCE FROM OIL SHALES IN AN OHIO COAL MINE
T120 The Structure of Faults from Top to Bottom: Implication for Fluid Flow, Ore Deposits, and Seismic Hazard (Posters)Monday, 20 October 20149:00 AM - 6:30 PMExhibition Hall C
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THREE-DIMENSIONAL GEOMETRY OF PSEUDOTACHYLYTE-BEARING FAULTS
8 Snoke Session 2: The Eclectic Tectonic Legacy of Arthur W. Snoke—Comparative Anatomy and Tectonic Evolution of Continental Margins from the Precambrian to Recent IMonday, 19 May 20141:00 PM - 5:00 PMGaines Hall 101
2013
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SMOOTH OPERATORS? ANALYSIS OF THE WORK BUDGET OF ROUGH FRICTIONAL FAULTS SUGGESTS THAT IT IS MECHANICALLY EFFICIENT FOR FAULTS TO MAINTAIN SOME DEGREE OF SELF-AFFINE ROUGHNESS
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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SANDSTONE INJECTITES RECORD PRE- AND SYN-FOLDING DEFORMATION AT SHEEP MOUNTAIN ANTICLINE, WYOMING
T369 Structural Geology and Geomechanics in the Petroleum Industry (Posters)Wednesday, 30 October 20139:00 AM - 6:30 PMHall D
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MICROROUGHNESS AND FRICTIONAL POWER DISSIPATION ON PSEUDOTACHYLYTE-BEARING FAULT SURFACES
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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DO FAULTS PRESERVE RECORDS OF THE SEISMIC CYCLE? 14 YEARS OF ADVANCEMENTS FROM FIELD OBSERVATIONS AND LABORATORY EXPERIMENTS
T216 The Rock Record of Fault Rheology and Slip Dynamics ITuesday, 29 October 20138:00 AM - 12:00 PMRoom 506
2012
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MICROROUGHNESS OF AN ANCIENT EARTHQUAKE FAULT
T85 Deformation Processes in Lithospheric High-Strain Zones IMonday, 5 November 20128:00 AM - 12:00 PM208A
2011
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DEFORMATION BANDS IN LARGE SANDSTONE DIKES NEAR SHEEP MOUNTAIN ANTICLINE, NORTH-CENTRAL WYOMING
73 Undergraduate Research IV (Posters)Tuesday, 22 March 20111:30 PM - 5:30 PMGrand Ballroom
2010
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DAMAGE ZONE CRACKS FORMED UNDER QUASI-STATIC AND DYNAMIC LOADING CONDITIONS: INSIGHTS FROM FIELD OBSERVATIONS, EXPERIMENTS, AND THEORY
T195 Where Does Earthquake Physics Meet Earthquake Geology? (Posters)Tuesday, 2 November 20108:00 AM - 6:00 PMHall D
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RECONSTRUCTING FEATURES OF EARTHQUAKE DYNAMICS FROM FIELD AND EXPERIMENTAL OBSERVATIONS
T173 Where Does Earthquake Physics Meet Earthquake Geology?Tuesday, 2 November 20108:00 AM - 12:00 PMLobby F
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QUANTIFYING THE STRUCTURE OF AN EXHUMED SEISMOGENIC FAULT ZONE USING DIFFERENTIAL GPS AND TERRESTRIAL LASER-SCANNING
T195 Where Does Earthquake Physics Meet Earthquake Geology? (Posters)Tuesday, 2 November 20108:00 AM - 6:00 PMHall D
2007
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PSEUDOTACHYLYTES IN FAULTS OF THE MT. ABBOT QUADRANGLE, SIERRA NEVADA: IMPLICATIONS FOR SEISMIC SLIP
T138 Recognition and Implications of Coseismic Fault-Zone Structures IITuesday, 30 October 20078:00 AM - 12:00 PM