oblique fault मीनिंग इन हिंदी

This fault is a reverse right-oblique fault.
In contrast, close to the FTFZ the terrain is more rugged and adorned with short, oblique fault scarps.
Some oblique faults occur within transpressional regimes, others occur where the direction of extension or shortening changes during the deformation but the earlier formed faults remain active.
Thus it appears that the Leech River and Devils Mountain faults were once a single left-lateral oblique fault ( having both horizontal strike-slip and vertical dip-slip motion ) that has been offset by right-lateral motion along the extended Survey Mountain Southern Whidbey Island Fault.