Yes, The plate boundary of the Jordan Dead Sea Transform Fault System (the Fault) is a clear example of this. The Arabian plate and Sinai-Palestine sub-plate are both moving Northwards. Arabia is moving faster than Sinai-Palestine so the fault is functioning in a left lateral strike slip fashion. With a rate of about 5 mm/yr. This is proved by evidences i.e. geological,, geophysical(aeromagnetic maps), seismological(focal mechanisms), from ArchaeoSeismology. Geomorphology, Geodesy (GPS monitoring).. etc.

Dear Dr. Najib https://www.researchgate.net/profile/Najib-Abou-Karaki

Maps on DST represent it as a left-lateral faulting in the sketch.

regards

ijaz

Strike-slip faults are vertical (or nearly vertical) fractures where the blocks have mostly moved horizontally. If the block opposite an observer looking across the fault moves to the right, the slip style is termed right lateral; if the block moves to the left, the motion is termed left lateral.

https://earthquake.usgs.gov › learn

Strike-Slip Fault - Earthquake Glossary

Well-known terrestrial examples include the San Andreas Fault, which, during the San Francisco earthquake of 1906, had a maximum movement of 6 metres (20 feet), and the Anatolian Fault, which, during the İzmit earthquake of 1999, moved more than 2.5 metres (8.1 feet).

https://www.britannica.com › science

strike-slip fault | Definition, Examples, & Locations | Britannica

https://www.britannica.com/science/strike-slip-fault,this link may be useful.

https://www.exploratorium.edu/faultline/basics/faults.html,this link may be useful.

The Arabian plate is bounded to the west versus the Levant Plate by the Dead-Sea transform fault. The fault separates the currently northward-moving Arabian Plate on its eastern side from the Levant Plate. The latter represents a northern extension of the African Plate on the western side. The movement started after the Cambrian Cu-Mn deposits (e.g., Timna) where emplaced in the Wadi Araba and some of its neighboring ones. Based upon these mineral deposits the displacement can clearly be determined.

DILL, H.G., BOTZ, R., BERNER, Z. and ABU HAMAD, A. M. B. (2010) The origin of pre – and syn-rift, hypogene Fe-P mineralization during the Cenozoic along the Dead-Sea-Transform Fault, Northwest Jordan.- Economic Geology, 105: 1301-1319.

I believe that most or all transform faults in the ocean do this; both sides are moving away from the mid-ocean ridge, but the velocities differ on either side of the transform fault.

Perhaps the specific movement of a tectonic vortex involves such a rupture style.

Yes, many---you can google slip rates on faults, but here's a great example:

Savage et al. 1990: Geodetic estimates of fault slip rates in the San Francisco Bay area. JGR v. 104, B3, pp 4995-5002. It shows how block displacement and hence slip rate on faults varies among the various subparallel strands of the SA fault system. Check out references therein, but if you get in touch i can provide quite a fe pdfs.

Different directions by same speed