Phase Transformations in Mantle Minerals
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Phase transformations in mantle minerals at high pressures                 and temperatures play a major role in the static and dynamic                    processes of the Earth's interior, especially in the transition                 zone from the upper to the lower mantle at depths between 350 and               700 km.  This action provides funds for support of research                     focused on two projects to study the properties and processes                   associated with these polymorphic phase transformations (1)                     Pressure dependence of the elastic properties of high-pressure                  phases; and (2) kinetics and mechanisms of phase transformations.               These experiments will be the large-volume, high-pressure                       facilities of the Stony Brook High Pressure Laboratory.
{'FirstName': 'Robert', 'LastName': 'Liebermann', 'PI_MID_INIT': None, 'PI_SUFX_NAME': None, 'PI_FULL_NAME': 'Robert Liebermann', 'EmailAddress': 'Robert.Liebermann@stonybrook.edu', 'NSF_ID': '000221269', 'StartDate': '02/01/1989', 'EndDate': None, 'RoleCode': 'Principal Investigator'}
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[{'Code': '1573', 'Text': 'Petrology and Geochemistry'}, {'Code': '1574', 'Text': 'Geophysics'}]
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