Slab temperature controls on the Tonga double seismic zone and slab mantle dehydration

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Slab temperature controls on the Tonga double seismic zone and slab mantle dehydration

Double seismic zones are two-layered distributions of intermediate-depth earthquakes that provide insight into the thermomechanical state of subducting slabs. We present new precise hypocenters of intermediate-depth earthquakes in the Tonga subduction zone obtained using data from local island-based, ocean-bottom, and global seismographs. The results show a downdip compressional upper plane and...

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Upper and mid‐mantle anisotropy beneath the Tonga slab

[1] Measurements of source‐side splitting in S waves from events within the Tonga slab reveal anisotropy in the upper and mid‐mantle beneath the slab. We observed splitting for events originating at both upper mantle and transition zone depths. Anisotropic fast directions ( ) are trench parallel or sub‐parallel for both upper mantle and transition zone events. Delay times (dt) decrease with dep...

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ژورنال

عنوان ژورنال: Science Advances

سال: 2017

ISSN: 2375-2548

DOI: 10.1126/sciadv.1601755