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Experimental study and active tectonics on the Zhangjiakou-Penglai fault zone across North China
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文摘

The ZPFZ controlled en échelon Quaternary pull-apart basins.

This lithospheric fault zone was seismogenic structure.

The experiment match well with actual earthquakes.

The seismic intensity is strong in the middle and weak at the two fault tips.

The ZPFZ is dominated by the combined effect of two geodynamic settings.

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