Meghan Miller, of Australian National University, will present this lecture.
Eastward along the Sunda-Banda arc, convergence transitions from subduction of oceanic lithosphere to arc-continent collision. This region of eastern Indonesia and Timor-Leste provides an opportunity for unraveling the processes that occur during collision between a continent and a volcanic arc, and can be viewed as the temporal transition of the process of continental collision along strike. We have collected a range of geological, geodetic, seismic, and geomorphic data to place constraints on the geometry and history of subduction.
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