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Tanya Furman is a geochemist and petrologist focused on fundamental questions related to whole Earth evolution. Her research addresses large-scale mass transfer that occurs in both deep and shallow regions of the mantle. Notable phenomena such as mantle plume activity, continental rifting, and plate convergence are closely examined in the context of inherited thermo-chemical structures within the deep Earth. She investigates the extent to which the mantle retains geochemically discrete reservoirs and the implications of chemical heterogeneities as evidenced in the compositions of mafic lavas. Her field research spans regions including East Africa, Turkey, and Saudi Arabia, where she assesses the geochemical impacts of lithospheric delamination linked to tectonic activities. Studies on the East African Rift System have provided insights into continental break-up and oceanic rift segmentation, utilizing structural and geochemical evidence. Additionally, she explores volcanic activity and geochemical feedback mechanisms critical to understanding Earth’s geological history, particularly regarding explosive volcanoes that pose risks to human life. Furman utilizes trace element and radiogenic isotopic signatures from volcanic rocks to analyze the evolution of the asthenosphere and lithosphere over geological time scales. Her academic journey includes a Ph.D. from the Massachusetts Institute of Technology and a BSE from Princeton University, coupled with previous teaching roles at the University of Virginia.
Penn State University • University Park, PA
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