I am interested in the role that mantle exhumation and serpentinization has on tectonic and geochemical processes. I use (U-Th)/He thermochronology and trace element geochemistry to 1) date magnetite that form during fluid alteration, 2) investigate the geochemical fingerprints of serpentinization at different tectonic settings, and 3) constrain the thermal history of ophiolites. My other work includes using (U-Th)/He techniques to study island arc exhumation and erosion, using a new sample set collected on a GEOPRISMS expedition to the Aleutians in 2015.
magnetite (u-th)/he thermochronology
Benchmark studies demonstrated that magnetite (U-Th)/He chronometry can be used to date volcanic and ore rocks.
I have tailored a method to date magnetite grains that form during serpentinization, the hydrous alteration of peridotite.
age of serpentinites
Serpentinites are found in relation to all types of plate boundaries. The timing of serpentinization, however, has been challenging to determine due to a lack of minerals with established dating techniques.
My approach is to use magnetite and spinel to date serpentinites from a variety of tectonic environments.
My field areas include the hyper-extended margin settings in the Swiss Alps and the Iberia-Newfoundland margin, an exhumed subduction complex in Syros, Greece, and the Oman ophiolite.
tectonic geochemical fingerprints
Serpentinites contain distinct geochemical fingerprints based on the melt history of the peridotite, and the composition of the serpentinizing fluid.
I am particularly interested in the mobility of uranium during serpentinization, and signatures of seawater alteration.