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Activity

2011

• USING HETEROGENEOUS QUARTZ CPO DATA TO INTERPRET THE DEFORMATION HISTORY OF A SHEAR ZONE AT THE BASE OF THE SEISMOGENIC ZONE
  T271 Constraints on Strain Rates, Stresses, and Deformation Processes During Shear Zone Localization at Different Lithospheric Levels
  Wednesday, 12 October 2011

  1:30 PM - 5:30 PM

  Room 200DE
• LITHODEMES, PSEUDOTACHYLYTE, ULTRAMYLONITE, MYLONITE AND STRIPED GNEISS WITHIN THE NORUMBEGA FAULT SYSTEM, SOUTH–CENTRAL AND CENTRAL MAINE
  68 Devonian Orogenesis in the Appalachian-Caledonian Mountain Belt—Where, When, and What Caused It?
  Tuesday, 22 March 2011

  1:30 PM - 5:35 PM

  Frick

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2010

• THE INFLUENCE OF PSEUDOTACHYLYTE FORMATION AND DEFORMATION ON BULK ROCK STRENGTH WITHIN A SHEAR ZONE FROM THE BASE OF THE SEISMOGENIC ZONE
  T173 Where Does Earthquake Physics Meet Earthquake Geology?
  Tuesday, 2 November 2010

  8:00 AM - 12:00 PM

  Lobby F

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2009

• MICROSTRUCTURAL RECORD OF COSEISMIC/POSTSEISMIC CYCLES NEAR THE BASE OF THE SEISMOGENIC ZONE, SAND HILL CORNER MYLONITE ZONE, NORUMBEGA FAULT SYSTEM, MAINE
  38 Rheology, Kinematics, and Strain Localization in Faults and Shear Zones II: NEtectonics
  Monday, 23 March 2009

  1:00 PM - 5:00 PM

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2008

• RHEOLOGICAL HETEROGENEITY AND THE STATE OF STRESS IN THE ROOTS OF A LARGE-DISPLACEMENT, STRIKE-SLIP, SEISMOGENIC FAULT: THE NORUMBEGA FAULT SYSTEM IN MAINE
  19 NEtectonics: The Implications of Crustal Heterogeneity for Structure, Rheology, and Tectonics II
  Friday, 28 March 2008

  8:00 AM - 9:40 AM