Evolution of the Ross Lake Fault Zone, North Cascades,      Washington
{'Code': '06030103', 'Directorate': {'Abbreviation': 'GEO', 'LongName': 'Directorate For Geosciences'}, 'Division': {'Abbreviation': 'EAR', 'LongName': 'Division Of Earth Sciences'}}
{'SignBlockName': 'Thomas O. Wright', 'PO_EMAI': None, 'PO_PHON': None}
Dextral strike-slip faults play a major role in the disruption of the           collage of accreted terranes in Washington and British Columbia.  The           major goal of this project is to place firm structural and geochronlogic        constraints on one of the major fault zone in this region, the Ross Lake        fault zone, which disrupts several terranes and was active during               metamorphism and plutonism in the adjacent crystalline core of the North        Cascades.  The kinematics of mylonite belts in the fault zone will be           determined through detailed mapping, study of small-scale structures and        kinematic indicators, while the timing of movement will be constrained          by dating plutonic bodies in the fault zone which show varying degrees          of deformation and metamorphism.  Results should substantially increase         knowledge of the late Mesozoic - early Cenozoic history of the                  crystalline core of the North Cascades.
{'FirstName': 'Robert', 'LastName': 'Miller', 'PI_MID_INIT': 'B', 'PI_SUFX_NAME': None, 'PI_FULL_NAME': 'Robert B Miller', 'EmailAddress': 'robert.b.miller@sjsu.edu', 'NSF_ID': '000234353', 'StartDate': '07/15/1987', 'EndDate': None, 'RoleCode': 'Principal Investigator'}
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{'Code': '157200', 'Text': 'Tectonics'}
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