Samuel H. Haines
Chevron Energy Technology Corporation, Houston, TX
Activity
2014
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PATHWAYS AND TIMING OF FLUID PULSES IN SHALLOW CRUSTAL FAULT SYSTEMS – H AND AR ISOTOPIC ANALYSIS OF NORMAL FAULTS IN THE SW US
T64 The Structure of Faults from Top to Bottom: Implication for Fluid Flow, Ore Deposits, and Seismic Hazard IISunday, 19 October 20141:00 PM - 5:00 PM118
2013
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REPEATING PATTERNS OF MINERAL TRANSFORMATIONS IN CLAY GOUGES, WITH EXAMPLES FROM LOW-ANGLE NORMAL FAULT ROCKS IN THE WESTERN USA
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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UNUSUAL ‘GRADED’ FAULT ROCKS FROM THE SNAKE RANGE DETACHMENT, NV –EVIDENCE BOTH FOR SEISMIC SLIP ON LOW-ANGLE NORMAL FAULTS AND PALEODIP AT THE TIME OF SLIP
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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CONNECTIONS BETWEEN FAULT ZONE STRENGTH, FABRIC, AND THE MODE OF FRICTIONAL SLIDING: LESSONS FROM EARTHSCOPE
304 125 Anniversary Pardee Symposium: Advances in Understanding Earth Structure and Process from EarthScopeWednesday, 30 October 20138:00 AM - 12:00 PMMile High Ballroom 4AB
2010
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LABORATORY MEASUREMENTS OF PERMEABILITY REDUCTION IN NATURALLY OCCURRING SHEAR BANDS FORMED IN UNLITHIFIED SANDS
33 Reservoir Characterization IIFriday, 28 May 20101:30 PM - 6:00 PMPlatinum 4
2009
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FAULT GOUGE AGES FROM THE SOUTH-CENTRAL PYRENEES FOLD-AND-THRUST BELT – DEMONSTRATION OF IN-SEQUENCE THRUSTING AND THE GEOLOGICAL SIGNIFICANCE OF WALL-ROCK PROVENANCE AGES EXTRAPOLATED FROM GOUGE DATING
T181 Linking Shallow to Deep Crustal Processes in Arc and Collisional Orogens (Posters)Tuesday, 20 October 20099:00 AM - 6:00 PMHall A
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UNUSUAL ‘GRADED' FAULT ROCKS FROM THE SNAKE RANGE DETACHMENT, NV – IMPLICATIONS FOR FLUID INVOLVEMENT IN LOW-ANGLE NORMAL FAULT PROCESSES AND THE ANGLE OF SLIP OF CORE COMPLEX DETACHMENTS
T12 Detachment Dynamics: Heat, Deformation, and Fluids in Extensional SystemsSunday, 18 October 20098:00 AM - 12:00 PMA107/108/109
2007
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CLAY FABRIC INTENSITY IN NATURAL AND EXPERIMENTAL CLAY-RICH FAULT ROCKS – IMPLICATIONS FOR CONDITIONS AND PROCESSES DURING FAULT SLIP
T105 Recognition and Implications of Coseismic Fault-Zone Structures IMonday, 29 October 20071:30 PM - 5:30 PM