Activity

2011

• THE SIGNIFICANCE OF STEEP REGIONAL FAULT AND SHEAR ZONES FOR THE DEVELOPMENT OF GNEISS DOMES WITHIN THE VARISCAN CORE ZONE OF THE PYRENEES: STRIKE-SLIP OR REVERSE FAULTS
  14 Significance of Large Strike-slip Fault Systems — Active and Ancient
  Monday, 5 September 2011

  2:00 PM - 5:10 PM

  A 017