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Experimental calibration of Fe and Mg partitioning between garnet and biotite samples at elevated pressures
Calibration, Metamorphism (Geology), Temperature measuring instruments, Garnet, Biotite, Geothermometry, Partitioning, Experiemental calibration
Geothermometers are natural mineral systems that may be used to estimate the temperatures that produce an equilibrated mineral assemblage in a metamorphic rock through element partitioning between minerals. This study is an experimental calibration of a garnet-biotite geothermometer using experimental methods based largely on Ferry and Spear's (1978) widely cited experimental calibration of a garnet-biotite geothermometer. This study used natural materials in order to better simulate metamorphic conditions. After a series of homogenization runs and experimental ion exchange runs at 600, 700 and 800°C this experiment has undergone entirely new reactions reflecting our simulated metamorphic conditions and resulting reactions of a pelitic amphibolite facies.
Durkin, Kathryn Elaine, "Experimental calibration of Fe and Mg partitioning between garnet and biotite samples at elevated pressures" (2012). Honors Project, Smith College, Northampton, MA.
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iii,, 45 p. : ill. (some col.) Honors project-Smith College, Northampton, Mass., 2012. Includes bibliographical references (p. 31-32)