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Activity

Date Unknown

• DUCTILE DEFORMATION OF WALL ROCK AT CONTACTS BETWEEN FERRAR DOLERITE SILLS AND BEACON SANDSTONE, DRY VALLEYS, ANTARCTICA: A CONSEQUENCE OF DISAGGREGATION AND RECEMENTATION IN SUPERCRITICAL FLUIDS DURING INTRUSION
  83 Structural Geology and Tectonics (Posters)
• DEFORMATION STYLE OF THE LEEDS-COXSACKIE SEGMENT OF THE HUDSON VALLEY FOLD-THRUST BELT
  9 Structural Geology and Tectonics (Posters)