The Chronology of the Development of the Montsec-Gavarnie   Structural Unit, South-Central Pyrenees, Northern Spain
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{'SignBlockName': 'Thomas O. Wright', 'PO_EMAI': None, 'PO_PHON': None}
The Pyrenees resulted from the collision between the Iberian               Peninsula and France.  The main phase of the Pyrenean orogeny in                northern Spain is characterized by the successive emplacement of                large thrust sheets into the south Pyrenean foredeep primarily                  during the early Tertiary.  In the zone ahead of the thrusts,s                  deformation of existing sediments, deposition of syntectonic                    conglomerates and formation of progressive unconformities in                    proximal sediments accompany thrust advancement.  This project                  will attempt to date thrust movement and to determine rates of                  thrusting by accurately dating these features.  Paleomagnetic                   stratigraphy techniques will be applied to date the syntectonic                 sediments and determine the extent of tectonic rotations that may               have occurred.  These results, in combination with structural and               biostratigraphic information, will be used to improve the                       synthesis of the development of the Pyrenean orogeny.
{'FirstName': 'Douglas', 'LastName': 'Burbank', 'PI_MID_INIT': 'W', 'PI_SUFX_NAME': None, 'PI_FULL_NAME': 'Douglas W Burbank', 'EmailAddress': 'burbank@eri.ucsb.edu', 'NSF_ID': '000117674', 'StartDate': '01/15/1989', 'EndDate': None, 'RoleCode': 'Principal Investigator'}
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[{'Code': '157100', 'Text': 'SCEC'}, {'Code': '157200', 'Text': 'Tectonics'}]
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