Ultralow velocity zone and deep mantle flow beneath the Himalayas are linked to a subducted slab

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Nature Geoscience | 2024年 / 17卷
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Through the detection of postcursors of shear waves diffracted at the core–mantle boundary, a zone of ultralow seismic velocities has been identified at the base of the mantle beneath the Himalayas. The presence of this zone is probably linked to a subducted slab remnant that is driving mantle flow in the region.
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