Halotectonic and Thrusting Processes in the Spanish Pyrnees
{'Code': '06030103', 'Directorate': {'Abbreviation': 'GEO', 'LongName': 'Directorate For Geosciences'}, 'Division': {'Abbreviation': 'EAR', 'LongName': 'Division Of Earth Sciences'}}
{'SignBlockName': 'Thomas O. Wright'}
The Pyrenees are an Alpine-age collisional orogen located                  along the border of the Iberian and European plates.  Associated                thrusting strongly affected sedimentation and the presence of                   salt beds produced an unusually well-developed set of structure                 that depend on a very weak layer.  This project is designed to                  address problems related to the interaction of thrusting, halo-                 tectonic and sedimentary events.  Results will be applicable to                 many collisional orogens in which salt beds are present.
{'FirstName': 'David', 'LastName': 'Anastasio', 'EmailAddress': 'dja2@lehigh.edu', 'StartDate': '04/01/1989', 'EndDate': None, 'RoleCode': 'Principal Investigator'}
{'Name': 'Lehigh University', 'CityName': 'Bethlehem', 'ZipCode': '180153005', 'PhoneNumber': '6107583021', 'StreetAddress': 'Alumni Building 27', 'CountryName': 'United States', 'StateName': 'Pennsylvania', 'StateCode': 'PA'}
{'Code': '1572', 'Text': 'Tectonics'}
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