The sedimentary history of the pull-apart basin faithfully records the strike-slip process of the faults that control the development of the pull-apart basins. The Banquan Basin is the largest and most typical pull-apart basin along the surface rupture zone of the 1668 Tancheng M8½ earthquake where the TLFZ shows the strongest seismic activity.
Click here for original story, When and how did dextral strike-slip movement of the Tanlu Fault Zone in the late Cenozoic occur?
Source: Phys.org