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Teyssier, C. and Tikoff, B. (1998) Strike-Slip Partitioned Transpression of the San Andreas Fault System: A Lithospheric-Scale Approach. In: Holdsworth, R.E., Strachan, R.A. and Dewey, J.F., Eds., Continental Transpressional and Transtensional Tectonics, Vol. 135, Geological Society of London Special Publication, London, 143-158.

has been cited by the following article:

• TITLE: Continental Transpression Evidence Checking along the Fault Dena: Iran, Middle Zagros

  AUTHORS: Ehsan Aziz, Mohsen Pourkermani, Korus Yazdjerdi, Ali Sorbi

  KEYWORDS: Dena Fault, Transpression, Strike-Slip, Zagros

  JOURNAL NAME: Open Journal of Geology, Vol.6 No.9, September 9, 2016

  ABSTRACT: Dena Fault is one of the fundamental and main structures with more than 130 km. One of the most important structural properties of this fault is changing in its trend so that at least three structural trends are detectable along this fault. Some continental transpression evidences along fault Dena are checked. These evidences are: Fold’s axis has configuration step and mutual desire. Fold’s axis average preferred orientation makes angles less than 45 degrees with preferred orientation of the boundary faults. Strike-slip faults are arranged overlapping and territory. P harmonic sections are more than harmonic sections R. In the central and southern parts the type is transpression Trust and in the northern part the type is transpression shear. In the present strike-slip component right lateral of this fault is dominant to its trust component and Fault function in the present era, is right lateral reverse.