A strength inversion origin for non-volcanic tremor
Non-volcanic tremor is a particularly enigmatic form of seismic activity. In its most studied subduction zone setting, tremor typically occurs within the plate interface at or near the shallow and deep edges of the interseismically locked zone. Detailed seismic observations have shown that tremor is...
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Springer Nature
2022
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| Online dostop: | https://nora.nerc.ac.uk/id/eprint/532590/1/s41467-022-29944-8.pdf |
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