RUI:  Structural and Metamorphic Evolution of the Eastern   Margin of the Coast Plutonic Complex East of Mt. Waddington,Southwestern British Columbia
{'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}
The Coast Plutonic Complex, an 1800 km long belt of                        Cretaceous and Tertiary metamorphic and plutonic rocks, straddles               the contact between the Insular and Intermontane super terranes in              British Columbia.  These allochthonous bodies were accreted either              during mid-Cretaceous time or possibly during the Jurassic.                          In order to help constrain models of the tectonic evolution                of the Coast Plutonic Complex, this project will examine the                    eastern margin of the belt in British Columbia where the                        structural and metamorphic history of this margin can be                        documented and the relative importance of transcurrent and thrust               faulting be assessed.  By providing information on the timing,                  style and regional extent of deformation and metamorphism, the                  project will contribute towards a comprehensive model for the                   origin of the belt and accretion of the Insular terrane.
{'FirstName': 'Margaret', 'LastName': 'Rusmore', 'PI_MID_INIT': 'E', 'PI_SUFX_NAME': None, 'PI_FULL_NAME': 'Margaret E Rusmore', 'EmailAddress': 'rusmore@oxy.edu', 'NSF_ID': '000448853', 'StartDate': '06/01/1988', 'EndDate': None, 'RoleCode': 'Principal Investigator'}
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{'Code': '9120', 'Text': 'CROSS-DIRECTORATE PROGRAMS'}
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