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- W2236214099 abstract "Subduction zone seismic structures at depths in the transition zone are reviewed. It has now been firmly established by seismic tomography that downgoing slabs from deep-sea trenches are deflected horizontally above the 660-km discontinuity and thus accumulate in the transition zone. Recent progress in seismic tomography reveals that once the slab penetrates the 660-km discontinuity, it is deflected subhorizontally in the uppermost lower mantle. Thus, the transition zone and the uppermost lower mantle together constitute a more or less laterally continuous reservoir of subducted slabs around the Circum-Pacific belt with a notable exception in Central America, where the slab descends deeper into the lower mantle. A remarkable correlation exists between the slab configuration and the deepest hypocentral distribution. A downgoing slab bent horizontally in the transition zone is marked by a subhorizontal bend of the deepest shock distribution. A penetrating slab subhorizontally deflected in the uppermost lower mantle is associated with a near-vertical alignment of the deepest hypocenters." @default.
- W2236214099 created "2016-06-24" @default.
- W2236214099 creator A5067709190 @default.
- W2236214099 creator A5074159971 @default.
- W2236214099 date "2015-01-01" @default.
- W2236214099 modified "2023-10-15" @default.
- W2236214099 title "Deep Earth Structure - Subduction Zone Structure in the Mantle Transition Zone" @default.
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- W2236214099 doi "https://doi.org/10.1016/b978-0-444-53802-4.00025-7" @default.
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