ROW:  Constraints on the Tectonic History of the Northern   Rio Grande Rift from Fission-Track Analysis
{'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 Rio Grande rift is an extensional tectonic feature                     located in Colorado and New Mexico.  Extensive research has                     established that the rift has been affected by two phases of                    deformation, each characterized by development of topography and                accompanied by volcanism.  Tectonic models have been developed                  using heat-flow, gravity, seismic and topographic information as                constraints. However, models for the earlier phase of deformation               are loosely constrained because the topographic parameters                      associated with the event are not well known.  This ROW project                 will employ fission-track analysis in order to provide better                   constraints on topographic relief and the near-surface cooling                  history of the Rio Grande Rift.
{'FirstName': 'Shari', 'LastName': 'Kelley', 'PI_MID_INIT': None, 'PI_SUFX_NAME': None, 'PI_FULL_NAME': 'Shari Kelley', 'EmailAddress': 'sakelley@gis.nmt.edu', 'NSF_ID': '000481291', 'StartDate': '06/15/1988', 'EndDate': None, 'RoleCode': 'Principal Investigator'}
{'Name': 'Southern Methodist University', 'CityName': 'DALLAS', 'ZipCode': '752051902', 'PhoneNumber': '2147684708', 'StreetAddress': '6425 BOAZ ST RM 130', 'StreetAddress2': None, 'CountryName': 'United States', 'StateName': 'Texas', 'StateCode': 'TX', 'CONGRESSDISTRICT': '24', 'CONGRESS_DISTRICT_ORG': 'TX24', 'ORG_UEI_NUM': 'D33QGS3Q3DJ3', 'ORG_LGL_BUS_NAME': 'SOUTHERN METHODIST UNIVERSITY', 'ORG_PRNT_UEI_NUM': 'S88YPE3BLV66'}
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{'Code': '1572', 'Text': 'Tectonics'}
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