Monazite Trace-Element and Isotopic Signatures of Ultrahigh- Pressure Metamorphism: Examples from the Western Gneiss Region, Norway
What Causes Ultrahigh-Temperature Metamorphism? A Case Study fromSouthern Madagascar
Metamorphic Petrology, Geochronology, Geochemistry
Alumni Graduate Award for Research Excellence, 2013/14
My research interests involve understanding how the continents of Earth have grown and changed through time. To address this question, I study metamorphic rocks from different places and times in Earth's history using fieldwork, petrography, radiometric dating, and phase-equilibria modeling. How/when did the rocks form and how/when were they brought to the surface? Are these processes the same today as they were in the past and if not, how are they different? How do these processes at depth influence what happens on the Earth's surface?
My current projects include studying the ultrahigh-temperature rocks of southern Madagascar (East African Orogeny, ~650-500 Ma) and the ultrahigh-pressure rocks from the Western Gneiss Region, Norway (Caledonian Orogeny, ~450-390 Ma).
EARTH 6: Mountains, Boots, and Backpacks (Teaching Assistant), F13
EARTH 102C: Metamorphic Petrology (Teaching Assistant), F12/F14
EARTH 104B: Field Methods (Teaching Assistant), S13/S14/S15
EARTH 114: Geomaterials (Teaching Assistant), W13
EARTH 115: Analytical Methods in Geomaterials (Teaching Assistant), W14
EARTH 118/119: Summer Field Geology (Teaching Assistant), M14