Seismic observation of the Earth's small-scale structure
The Earth’s mantle is chemically and thermally heterogeneous varying in 3-dimensions and on many length-scales. Subduction introduces slabs into the mantle while interactions with the core may enrich the mantle in iron. The lower mantle demonstrates the strongest seismic anomalies outside of the cru...
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University of Leeds
2014
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.617317 |