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Lithospheric rheology and Moho upheaval control the generation mechanism of the intraplate earthquakes in the North China Basin
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文摘

Large earthquakes occurred in the regions where Moho upheaves in the NCB.

Interseismic crustal stress accumulation is simulated under the condition of compression.

Stress concentration in the regions where Moho upheaves is responsible for the earthquakes.

Both lithospheric rheology and Moho upheaval control the stress accumulation process.

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