COLLABORATIVE RESEARCH:  Paleomagnetic Investigation of Late Cretaceous and Early Tertiary Volcanic Rocks
{'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 apparent polar wander path for North America during the                Late Cretaceous to Paleocene interval contains a deflection or                  cusp that may reflect a period of major plate reorganization.                   However, the resolution of the APW is insufficient to demonstrate               that portions on either side of the cusp are small circle paths                 and that the cusp is a distinct break.  This project will utilize               several volcanic sequences of Late Cretaceous to Eocene age in                  Montana to refine, using standard paleomagnetic techniques, the                 North American Late Cretaceous  apparent polar wander path.  The                work will be conducted in collaboration with researchers at the                 Michigan Technological University.
{'FirstName': 'Steven', 'LastName': 'Sheriff', 'PI_MID_INIT': 'D', 'PI_SUFX_NAME': None, 'PI_FULL_NAME': 'Steven D Sheriff', 'EmailAddress': 'GL SDS@SELWAY.UMT.EDU', 'NSF_ID': '000428081', 'StartDate': '06/01/1988', 'EndDate': None, 'RoleCode': 'Principal Investigator'}
{'Name': 'University of Montana', 'CityName': 'MISSOULA', 'ZipCode': '598120003', 'PhoneNumber': '4062436670', 'StreetAddress': '32 CAMPUS DR', 'StreetAddress2': None, 'CountryName': 'United States', 'StateName': 'Montana', 'StateCode': 'MT', 'CONGRESSDISTRICT': '00', 'CONGRESS_DISTRICT_ORG': 'MT00', 'ORG_UEI_NUM': 'DAY7Z8ZD48Q3', 'ORG_LGL_BUS_NAME': 'UNIVERSITY OF MONTANA', 'ORG_PRNT_UEI_NUM': None}
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{'Code': '1572', 'Text': 'Tectonics'}
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