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That is one reason why understanding the complexities of the fault structure is important.
Dominant fault zones have depths 1,136.
Misfaq-Bardawil (Temsah) fault appears to be active only since Miocene: The dominant fault movement is due to the pre-salt including post-salt reactivation.
The continuous subsurface fault structure along the Futagawa fault zone is clearly detected with HD, VD and TDX.
This implies a complex fault structure along the Futagawa Hinagu fault system.
Figure 1 Geological map of central Taiwan, an E-W cross section through site, and three dominant fault zones discovered.
We assume this N-S striking plane to be the dominant fault plane in the earthquake sequence.
It is indicated that both the fault structures and the alteration contact zones are well developed as the dominant engineering geological characteristics in the Jinchuan mine areas.
Of these four, two have dominant faults that dip southeast and the other two have dominant faults dipping northwest.
Ambiguous stratigraphic correlation or inconsistency of fault-displacement accumulation on both sides of the dominant faults.
In addition, note that in seismic transect B–B', the dominant fault-throw direction of the faults at base Eagle Ford Shale (red) is NW, whereas the fault-throw direction of faults within the Austin Chalk (black) is SE.
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