Evidence of Non-Dipole Fields in the Paleomagnetic Record ofDeep-Sea Sediments
{'Code': '06040200', 'Directorate': {'Abbreviation': 'GEO', 'LongName': 'Directorate For Geosciences'}, 'Division': {'Abbreviation': 'OCE', 'LongName': 'Division Of Ocean Sciences'}}
{'SignBlockName': 'Bilal U. Haq', 'PO_EMAI': None, 'PO_PHON': None}
The PI proposes to study departures of the geomagnetic field from               the geocentric axial dipole which provides a very good model for                the Earth's magnetic field.  These departures from the dipole                   field model will be determined in sedimentary cores and will be                 used to model the contribution of small scale changes in the                    Earth's magnetic field for the last 5 million years.  This work                 is a continuation of earlier work in the equatorial Indian and                  Atlantic Oceans; the PI proposes to identify still smaller                      deviations of the magnetic field by studying higher latitude                    cores where that effect is best seen.  This study in combination                with the earlier work will provide a fine-scale analysis of the                 magnetic field behaviour of the Earth.
{'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': '11/15/1987', '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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