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Seismic evidence for a tilted mantle plume and north-south mantle flow beneath Iceland

机译:冰岛下方的地幔柱倾斜和南北地幔流动的地震证据

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摘要

Shear waves converted from compressional waves at mantle discontinuities near 410- and 660-km depth recorded by two broadband seismic experiments in Iceland reveal that the center of an area of anomalously thin mantle transition zone lies at least 100 km south of the upper-mantle low-velocity anomaly imaged tomographically beneath the hotspot. This offset is evidence for a tilted plume conduit in the upper mantle, the result of either northward flow of the Icelandic asthenosphere or southward flow of the upper part of the lower mantle in a no-net-rotation reference frame.
机译:冰岛两次宽带地震实验记录的在410和660 km附近的地幔不连续处的压缩波转换而成的剪切波显示,异常稀薄的地幔过渡带区域的中心位于上地幔低点以南至少100 km速度断层成像在热点下方的速度异常。此偏移量是上地幔中羽状导管倾斜的证据,这是在无网旋转参考系中冰岛软流圈向北流动或下地幔上部向南流动的结果。

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