Activity

2015

• ION MICROPROBE δ18O-CONSTRAINTS ON FLUID MOBILITY AND THERMAL STRUCTURE DURING EARLY SLIP ON A LOW-ANGLE NORMAL FAULT, CHEMEHUEVI MOUNTAINS, SE CA
  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