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• W1988393860 abstract "[1] The occurrence of seismic anisotropy in the Earth's upper mantle is a global phenomenon related to subcrustal deformation and flow processes. The shear wave splitting analysis method has led to a global set of anisotropy maps mainly derived from receiver-side analysis. Remote places with few seismometers deployed remain unexamined. Source-side splitting analysis allows mapping of mantle fabrics in these regions. Here, we investigate seismic anisotropy in the South Sandwich Islands subduction environment. Core-reflected ScS waves recorded at the Neumayer seismograph network are corrected for well constrained receiver anisotropy and then analysed for source anisotropy. Sub-slab mantle minerals are aligned horizontally almost parallel to the trench indicating a westward flow around the subducting slab. This is consistent with a model of horizontal mantle flow due to slab rollback that was previously inferred from marine and geochemical studies in the back-arc region." @default.
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• W1988393860 date "2008-02-13" @default.
• W1988393860 modified "2023-10-10" @default.
• W1988393860 title "Mantle flow in the South Sandwich subduction environment from source-side shear wave splitting" @default.
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• W1988393860 doi "https://doi.org/10.1029/2007gl032411" @default.
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