Width and Displacement Values

Most of the fault zones in this survey are commonly steep in the seismic section and present as slightly normal throws. The throw is used as a proxy for displacement in this research. We measured the W-D data set at almost all fault zones by the 90 numbered seismic sections from the TVSS structure map co-rendered with the FPC attribute indicating the fault traces. The boundary of the displayed FCB attribute is considered the boundary of the fault zone. Thus, it is easily taken as the united identification criterion in this research. Fault zone W-D measurements were taken every 350 m along every single fault trace from northeast towards southwest.