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Activity

2013

• DAMAGE, PERMEABILITY AND SEALING PROCESSES OF AN EXHUMED SEISMIC FAULT ZONE; THE GOLE LARGHE FAULT ZONE, ITALIAN ALPS
  T326 Structure and Evolution of Brittle Faults and Fault Rocks: Physical Properties, Geometry, and Geochemical Changes that Influence Water, Energy, and Mineral Resources
  Wednesday, 30 October 2013

  8:00 AM - 12:00 PM

  Room 507
• 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 Resources
  Wednesday, 30 October 2013

  8:00 AM - 12:00 PM

  Room 507

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2012

• MICROROUGHNESS OF AN ANCIENT EARTHQUAKE FAULT
  T85 Deformation Processes in Lithospheric High-Strain Zones I
  Monday, 5 November 2012

  8:00 AM - 12:00 PM

  208A

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2010

• RECONSTRUCTING FEATURES OF EARTHQUAKE DYNAMICS FROM FIELD AND EXPERIMENTAL OBSERVATIONS
  T173 Where Does Earthquake Physics Meet Earthquake Geology?
  Tuesday, 2 November 2010

  8:00 AM - 12:00 PM

  Lobby F
• PRINCIPAL SLIP ZONES IN LIMESTONE: NATURAL AND EXPERIMENTAL EXAMPLES AND IMPLICATIONS FOR THE SEISMIC CYCLE
  T173 Where Does Earthquake Physics Meet Earthquake Geology?
  Tuesday, 2 November 2010

  8:00 AM - 12:00 PM

  Lobby F
• 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 2010

  8:00 AM - 6:00 PM

  Hall D
• THE SEISMIC CHARACTER OF MELANGE ZONES: RECORD OF MEGA-EARTHQUAKES IN THE KODIAK ACCRETIONARY COMPLEX, PASAGSHAK POINT, KODIAK IS., ALASKA
  41 Modern accretionary wedges and ancient analogues
  Friday, 8 October 2010

  9:30 AM - 12:30 PM

  Kemal Kurdas Salon

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2007

• PSEUDOTACHYLYTES IN FAULTS OF THE MT. ABBOT QUADRANGLE, SIERRA NEVADA: IMPLICATIONS FOR SEISMIC SLIP
  T138 Recognition and Implications of Coseismic Fault-Zone Structures II
  Tuesday, 30 October 2007

  8:00 AM - 12:00 PM
• UNRAVELING SEISMIC DEFORMATION IN EXHUMED SUBDUCTION THRUSTS: THE ULTRAFINE-GRAINED FAULT ROCKS OF PASAGSHAK POINT, KODIAK ISLAND, AK
  T138 Recognition and Implications of Coseismic Fault-Zone Structures II
  Tuesday, 30 October 2007

  8:00 AM - 12:00 PM

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2003

• SUPERHEATED FRICTION-INDUCED MELTS IN ZONED PSEUDOTACHYLYTES WITHIN THE ADAMELLO TONALITES (ITALIAN SOUTHERN ALPS)
  T249 Seismogenic Friction and Pseudotachylites
  Wednesday, 5 November 2003

  1:30 PM - 5:30 PM
• TRANSITION FROM CATACLASITES TO PSEUDOTACHYLYTES AND CONSEQUENCES ON THE MESOSCOPIC STRUCTURE OF A “STRONG-TYPE” SEISMOGENIC FAULT
  T249 Seismogenic Friction and Pseudotachylites
  Wednesday, 5 November 2003

  1:30 PM - 5:30 PM