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GEOLOGICAL SCIENCES AT BROWN UNIVERSITY Another important focus is the use of seismic velocity anomalies and anisotropy to help map flow in the mantle. Seismic anisotropy in the upper mantle is likely caused by shearing due to plate motions and convection, with additional influence from partial melt in certain regions. With the aid of theoretical models of convection and wave propagation, we are studying mantle structure and flow near subduction zones and mid-ocean ridges, beneath continents, and at the core-mantle boundary. Unique data sets of seismic waveforms have been acquired in the TUCAN, GLIMPSE, MELT, MOMA (Missouri to Massachusetts), NOMAD and FLED (Florida to Edmonton) Experiments. These examples show how integration of theory and observation is fundamental to the philosophy of our group. Our mode of research emphasizes collaboration. Students typically work with more than one of our faculty, and we enjoy an interactive environment that includes seminars, informal research talks and lots of discussion. Our mode of research emphasizes collaboration. Students typically work with more than one of our faculty, and we enjoy an interactive environment that includes seminars, informal research talks and lots of discussion. |
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