David A. Lockner
U. S. Geological Survey, Menlo Park, CA
Activity
2023
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CHEMICAL AND PHYSICAL PROPERTIES OF CORE FROM SERPENTINITE MUD VOLCANOES, NORTHERN MARIANA SUBDUCTION ZONE
31 Tectonic Processes along Subduction Zone Margins (Posters)Friday, 19 May 20238:00 AM - 6:00 PMCargo Room
2018
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COMPOSITION AND STRENGTH OF ULTRAMAFIC-RICH GOUGE FROM THE BARTLETT SPRINGS FAULT, CALIFORNIA COMPARED TO SAFOD GOUGES: IMPLICATIONS FOR FAULT CREEP
47 D38. Structural Geology (Posters)Sunday, 4 November 20189:00 AM - 5:30 PMHalls J-K
2017
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THE INFLUENCE OF METASOMATIC ALTERATION ON THE FRICTIONAL PROPERTIES OF SERPENTINITE-BEARING GOUGE IN THE BARTLETT SPRINGS FAULT, NORTHERN CALIFORNIA
T288 Challenges in Tectonics: Fault Zone Behavior through Time, from Earth’s Surface to the Upper Mantle (Posters)Tuesday, 24 October 20179:00 AM - 6:30 PMHalls 4EF
2015
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AN EXPERIMENTAL STUDY ON EVOLUTION OF FRACTURE PERMEABILITY OF ULTRAMAFIC ROCKS DURING SERPENTINIZATION REACTIONS
326 Geophysics/GeodynamicsWednesday, 4 November 20151:30 PM - 5:30 PMRoom 322/323
2013
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CHEMOMECHANICAL CONTROLS ON CREEP PROCESSES IN THE SAN ANDREAS FAULT REVEALED IN SAFOD CORE
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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FAULT WEAR EXPERIMENTS, PART II: TRANSIENT AND STEADY-STATE STAGES UNDER EARTHQUAKE-LIKE SLIP-VELOCITY HISTORY
T195 Where Does Earthquake Physics Meet Earthquake Geology? (Posters)Tuesday, 2 November 20108:00 AM - 6:00 PMHall D
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FAULT WEAR EXPERIMENTS, PART I: TRANSIENT AND STEADY-STATE STAGES UNDER CONSTANT SLIP-VELOCITY
T195 Where Does Earthquake Physics Meet Earthquake Geology? (Posters)Tuesday, 2 November 20108:00 AM - 6:00 PMHall D
2009
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INFLUENCE OF FLUID CHEMISTRY ON THE FRICTIONAL BEHAVIOR OF ULTRAMAFIC ROCKS
T157 Geofluids and Deformation: Integrated Studies for the 21st CenturyTuesday, 20 October 20098:00 AM - 12:00 PMA105
2008
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The Influence of Clay Authigenesis on the Mechanical and Hydrological Properties of the Moab Fault, Utah
T290 Brittle Deformation and Diagenesis as Coupled ProcessesWednesday, 8 October 20088:00 AM - 12:00 PM
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Large-Scale Continental Deformation: Fluid-Rock Interaction and Compartmentalization along the San Andreas Fault at SAFOD
204 Geophysics/Tectonophysics/SeismologyMonday, 6 October 20081:30 PM - 5:30 PM
2005
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TALC FRICTION AT ELEVATED TEMPERATURES AND PRESSURES: A VERY WEAK MINERAL THROUGHOUT THE SEISMOGENIC ZONE
237 Geophysics/Tectonophysics/SeismologyWednesday, 19 October 20051:30 PM - 5:30 PM
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FAULT ROCK GENERATION, FRICTIONAL PROPERTIES, AND PERMEABILITY IN FAULT ROCKS OF THE MOAB FAULT, UTAH
T226 Fracturing and Faulting of the Clastic Rocks of the Colorado PlateauWednesday, 19 October 20058:00 AM - 10:00 AM
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FORMATION AND RHEOLOGICAL IMPLICATIONS OF CLAY-BEARING FAULT ROCKS OF THE MOAB FAULT SYSTEM, UTAH
T226 Fracturing and Faulting of the Clastic Rocks of the Colorado PlateauWednesday, 19 October 20058:00 AM - 10:00 AM
2002
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MAPPING THE COEFFICIENT OF FRICTION OF THE SERPENTINE MINERAL CHRYSOTILE RELATIVE TO EFFECTIVE NORMAL STRESS AND TEMPERATURE
6 Geophysics/Tectonophysics/SeismologySunday, 27 October 20028:00 AM - 12:00 PM
Date Unknown
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DISPROPORTIONATE WEAKENING OF SERPENTINITE FAULT GOUGE BY TALC AND BRUCITE
173 Geophysics/Tectonophysics/Seismology (Posters)
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FRICTION OF 2:1 SHEET SILICATES - HOW CRYSTAL STRUCTURE INFLUENCES SHEAR STRENGTH
T262 Phase Relations, High P-T Terrains, P-T-ometry and Plate Pushing (Posters): A Tribute to W.G. Ernst