Asthenospheric channeling of the Icelandic upwelling: Evidence from seismic anisotropy
Two end-member geometries, radial flow and ridge-channeled flow, have been proposed for the dispersion of material upwelling beneath Iceland. Seismic anisotropy provides information on mantle flow, and therefore has the potential to discriminate these two geometries. In this study, we combine the HO...
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| Format: | Text |
| Language: | English |
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2005
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.412.71 http://seismo.berkeley.edu/~rallen/pub/2004xue/2005_XueAllen_IcelandSplits_EPSL.pdf |