Kinematic Analysis of a Major Fault System in the Blue RidgeProvince, Southern and Central Appalachians
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{'SignBlockName': 'Thomas O. Wright', 'PO_EMAI': None, 'PO_PHON': None}
Recent kinematic studies of major faults in the Blue Ridge                 of southwestern Virginia have raised the possibility that many of               these faults were extensional during the late Precambrian and                   were then locally reactivated during Paleozoic compression.                     Extensive mylonitic tectonic fabrics record sense of shear and                  relic peak metamorphic assemblages record conditions in the foot-               wall and hanging wall of the fault systems.  Results will                       rigorously test the hypothesis for early, major extensional                     tectonics prior to the Paleozoic closure of Iapetus.
{'FirstName': 'Carol', 'LastName': 'Simpson', 'PI_MID_INIT': None, 'PI_SUFX_NAME': None, 'PI_FULL_NAME': 'Carol Simpson', 'EmailAddress': 'csimpson@wpi.edu', 'NSF_ID': '000110412', 'StartDate': '11/01/1988', 'EndDate': None, 'RoleCode': 'Principal Investigator'}
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{'Code': '1572', 'Text': 'Tectonics'}
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