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沿消减带的某些板块边界似乎长期无震。
Certain parts of the plate boundaries along subduction zones appear to be aseismic.
消减带岩片带入的组分。
对全球不同区域的地震静态应力触发情况的研究表明，消减带“地震对”的触发效应较为明显。
The research on seismic static stress triggering in different regions in the world indicates that triggering effect is significant in subduction belts.
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