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The Mw7.9 2014 intraplate intermediate-depth Rat Islands earthquake and its relation to regional tectonics
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文摘

The causative fault plane is steeply-dipping (87°) based on the relocated aftershocks.

The 2014 earthquake breaks the entire elastic core of the subducting slab.

The seismic cycle is similar for intermediate-depth and interplate earthquakes.

Intermediate-depth earthquakes contribute to the block motion in Central Aleutian.

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