Configuration of the Time-Averaged Geomagnetic Field from   the Global Deep-Sea Sediment Record
{'Code': '06030204', 'Directorate': {'Abbreviation': 'GEO', 'LongName': 'Directorate For Geosciences'}, 'Division': {'Abbreviation': 'EAR', 'LongName': 'Division Of Earth Sciences'}}
{'SignBlockName': 'Michael A. Mayhew', 'PO_EMAI': None, 'PO_PHON': None}
The PI will examine any polarity asymmetry in deep-sea sediment                 paleomagnetic data from intermediate latitudes (north and south)                to determine the actual configuration of the standing non-dipole                field.  Better characterization of persistent and polarity-                     dependent non-dipole field components is directly relevant to our               understanding of the behavior of the geomagnetic field during                   polarity transitions, is needed for high resolution plate                       tectonic and true polar wander studies, and may lend greater                    insight as to the physical source(s) of field generation.
{'FirstName': 'Dennis', 'LastName': 'Kent', 'PI_MID_INIT': 'V', 'PI_SUFX_NAME': None, 'PI_FULL_NAME': 'Dennis V Kent', 'EmailAddress': 'dvk@ldeo.columbia.edu', 'NSF_ID': '000543500', 'StartDate': '03/15/1989', 'EndDate': None, 'RoleCode': 'Principal Investigator'}
{'Name': 'Columbia University Lamont Doherty Earth Observatory', 'CityName': 'Palisades', 'CountyName': None, 'ZipCode': '10964', 'PhoneNumber': '9143592900', 'StreetAddress': 'Rt 9W', 'StreetAddress2': None, 'CountryName': 'United States', 'StateName': 'New York', 'StateCode': 'NY', 'CONGRESSDISTRICT': '17', 'CONGRESS_DISTRICT_ORG': 'NY17', 'ORG_DUNS_NUM': '130479392', 'ORG_LGL_BUS_NAME': None, 'ORG_PRNT_DUNS_NUM': None}
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[{'Code': '1574', 'Text': 'Geophysics'}, {'Code': '1620', 'Text': 'Marine Geology and Geophysics'}]
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