▁developed ▁features ▁include ▁trans position ▁fol i ations , ▁line ations , ▁st yl ol ites , ▁fol ds , ▁and ▁reverse ▁fault s . ▁P ure ▁she ar - domin ated ▁trans pression ▁usually ▁gives ▁ste ep ▁line ations , ▁while ▁simple ▁she ar - domin ated ▁trans pression ▁fav ors ▁horizontal ▁line ations . ▁It ▁is ▁also ▁common ▁for ▁non - vertical ▁trans pression al ▁zones ▁to ▁have ▁a ▁significant ▁component ▁of ▁she aring ▁parallel ▁to ▁the ▁di pl ine ▁of ▁the ▁zone ▁boundary . ▁In ▁these ▁zones , ▁the ▁line ations ▁are ▁between ▁horizontal ▁and ▁vertical . ▁The ▁complete ▁geometry ▁presented ▁by ▁all ▁struct ural ▁elements ▁in ▁the ▁zone ▁is ▁used ▁to ▁const rain ▁the ▁actual ▁boundary ▁disp lac ements . ▁. ▁ ▁R estra ining ▁b end ▁ ▁A ▁fault ▁b end , ▁or ▁fault ▁step over , ▁forms ▁when ▁individual ▁segments ▁of ▁the ▁fault ▁overlap ▁and ▁link ▁together . ▁The ▁type ▁of ▁structures ▁which ▁form ▁along ▁the ▁strike - s lip ▁fault ▁depend ▁on ▁the ▁sense ▁of ▁s lip ▁relative ▁to ▁the ▁sense ▁of ▁ste pping . ▁When ▁a ▁sin ist ral ▁fault ▁steps ▁to ▁the ▁right ▁or ▁a ▁de xt ral ▁fault ▁steps ▁to ▁the ▁left , ▁a ▁rest ra ining ▁b end ▁is ▁formed . ▁These ▁are ▁areas ▁of ▁positive ▁relief ▁( top ographic ▁u pl ift ), ▁cr ust al ▁short ening , ▁and ▁ex hum ation ▁of ▁cry st all ine ▁bas ement . ▁As ▁seen ▁in ▁deeply ▁er oded ▁out c rop ▁expos