Relationships Between Neogene Volcanism, Basin Evolution,   and Extensional Faulting:  Death Valley - Panamint Valley   Area, California
{'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}
Sedimentary basins are among the most conspicuous results of               Neogene continental extension in the North American Cordillera,                 however, the connection between structural development and                      sedimentologic response is less than clear.  This project will                  take advantage of an uplifted and dissected late Miocene-Pliocene               extensional basin exposed in the Panamint Valley and Death Valley               area of southeastern California.  The work will involve mapping,                chemical analysis, sedimentology and age dating techniques to                   establish the structural history and associated sedimentologic                  response.  Results will provide an added dimension to the subject               of extensional tectonics.
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{'Name': 'Massachusetts Institute of Technology', 'CityName': 'CAMBRIDGE', 'ZipCode': '021394301', 'PhoneNumber': '6172531000', 'StreetAddress': '77 MASSACHUSETTS AVE', 'StreetAddress2': None, 'CountryName': 'United States', 'StateName': 'Massachusetts', 'StateCode': 'MA', 'CONGRESSDISTRICT': '07', 'CONGRESS_DISTRICT_ORG': 'MA07', 'ORG_UEI_NUM': 'E2NYLCDML6V1', 'ORG_LGL_BUS_NAME': 'MASSACHUSETTS INSTITUTE OF TECHNOLOGY', 'ORG_PRNT_UEI_NUM': 'E2NYLCDML6V1'}
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[{'Code': '1571', 'Text': 'SCEC'}, {'Code': '1572', 'Text': 'Tectonics'}]
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