Intraplate strike-slip zones commonly display intricate 3-D geometries, with rapid changes in
structural style along strike and with depth. Strike-slip deformation typically results in …

The Dead Sea Fault is an active transform fault linking opening in the Red Sea with collision
in the Taurus/Zagros Mountains. Motion is left-lateral and estimated at approximately 5–7 …

Turkey forms one of the most actively deforming regions in the world and has a long history
of devastating earthquakes. The belter understanding of its neotectonic features and active …

We here summarize the evolution of the greater Red Sea–Gulf of Aden rift system, which
includes the Gulfs of Suez and Aqaba, the Red Sea and Gulf of Aden marine basins and …

The structures along the Dead Sea transform (rift) are related to the motions of the Sinai and
Arabia plates which border it, and to the irregularities of their boundaries. The total slip was …

Strike-slip fault systems often contain zones of steep imbricate faults geometrically similar to
imbricate fans and duplexes in dip-slip, thrust and normal, fault systems. They are evident in …

A comparative study of well mapped active and ancient pull-apart basins suggests a
qualitative model for their continuous development. Pull-aparts evolve from incipient to …

The reconstruction of ancient marine environments is an important task of the Earth
Sciences, of great interest to geology, pure and applied, to oceanography and climatology …

Pull‐apart basins or rhomb grabens and horsts along major strike‐slip fault systems in the
world are generally associated with horizontal slip along faults. A simple model suggests …

Abstract Manifestations of Late Quaternary and Holocene faulting were studied in a 500 km
long segment of the Dead Sea transform (rift). Most prominent are left-slip faults, whose …