Activity

2015

• 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 2015

  9:00 AM - 6:30 PM

  Exhibit Hall
• 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 2015

  9:00 AM - 6:30 PM

  Exhibit Hall