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THE NORTH ANATOLIAN FAULT ZONE - DISTRIBUTED NEOGENE DEFORMATION IN ITS NORTHWARD CONVEX PART
(ELSEVIER SCIENCE BV, 1995)
The North Anatolian Fault Zone is composed of two almost rectilinear branches which join in a northward convex bend. In this bent zone, the Pontide-Anatolide collisional system has been cut across by two transpressional ...
POST-TORTONIAN WESTWARD AND SOUTHWARD THRUSTING IN THE CORE OF THE ISPARTA REENTRANT (TAURUS, TURKEY) - GEODYNAMIC IMPLICATIONS
(SOC GEOL FRANCE, 1995)
The Isparta re-entrant (Taurus, Turkey), is made up two converging thrust-systems resulting from rotations in opposite sense. In this paper, we focus on the tectonic history post-dating the rotations. Kinematic analysis ...