COLLABORATIVE RESEARCH:  Lateral Variations in the Timing   and Nature of Metamorphism Associated With A Major Terrane  Boundary in the NW Himalaya
{'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 Main Mantle Thrust, located in the northwestern Himalaya               of Pakistan, separates the Kohistan island-arc terrane on the                   north from the Indian plate to the south, and represents the                    westward continuation of the Indus Suture zone into the western                 Himalaya.  The focus of this collaborative project (with Lehigh                 University, EAR88-16887) is to examine metamorphism associated                  with the terrane boundary to establish pressure-temperature-time                paths and radiometric dates of structural events.  Data obtained                using these techniques will be integrated to place important                    constraints on tectonic-thermal models for the Himalaya, and                    compressional mountain belt in general.
{'FirstName': 'C. Page', 'LastName': 'Chamberlain', 'PI_MID_INIT': None, 'PI_SUFX_NAME': None, 'PI_FULL_NAME': 'C. Page Chamberlain', 'EmailAddress': 'chamb@stanford.edu', 'PI_PHON': '6507256835', 'NSF_ID': '000178932', 'StartDate': '03/15/1989', 'EndDate': None, 'RoleCode': 'Principal Investigator'}
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{'Code': '1572', 'Text': 'Tectonics'}
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