2019 Geology Colloquium Series
Friday, April 26th 2019 at 3:10 pm
in PLS 1140
Watch live at https://www.geol.umd.edu/youtube
Johns Hopkins University
Metamorphism and the Evolution of Plate Tectonics
At present, Earth’s mantle convection, which facilitates planetary heat loss, is expressed at the surface as plate tectonics. When plate tectonics emerged and how it has evolved through time are two of the most fundamental and provocative questions outstanding in Earth science. Metamorphic rocks, those that have experienced solid-state mineral transformations due to changes in pressure (P) and temperature (T), record periods of burial/exhumation and heating/cooling that reflect the tectonic environments in which they formed. Changes in the global distribution of metamorphic P–T conditions in the continental crust through time reflect secular evolution of Earth’s tectonic processes at convergent plate boundaries. On modern Earth, convergent plate margins are characterized by metamorphic rocks that record a bimodal distribution of apparent thermal gradients (change in temperature with depth, parameterized in this talk as metamorphi! c T/P), in the form of paired metamorphic belts, which is attributed to metamorphism near to (low T/P) and away from (high T/P) subduction zones. In this talk, I will evaluate the emergence of bimodal metamorphism as a proxy for secular change in plate tectonics using a statistical evaluation of the distributions of metamorphic T/P through time. I will argue that Earth’s modern plate tectonic regime developed gradually since the Neoarchaean Era in conjunction with secular cooling of the mantle and associated changes in the thickness, buoyancy and rheology of oceanic lithosphere, resulting in an evolution in the styles of both subduction and collisional orogenesis.