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The Taihang Mountain piedmont fault is a large-scale structure zone in north and east China which cross Beijing, with the NE-NNE extent spans approximately 620 km. It is very important to determine the fault zone activity due to the close relation of active structures and earthquakes. Regarding the fault activity, there are three different opinions: 1) it is a large deep fault zone; 2) it is an active...
Seismic method is one of the main tools of assessing fault activity. There are P-wave reflection and shear-wave splitting methods when active fault is investigated using seismic methods. The P-wave reflection method is according to the fact that whether bedrock fault extends up to Quaternary strata Q3 or not, while shear-wave splitting method is according to anisotropy of Quaternary strata Q3 determined...
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