Browsing by Author "Unlugenc, Ulvi Can"
Now showing items 1-5 of 5
-
Late cenozoic stress field in the Cameli Basin, SW Turkey
Over, Semir; Pinar, Ali; Ozden, Suha; Yilmaz, Huseyin; Unlugenc, Ulvi Can; Kamaci, Zuheyr (ELSEVIER SCIENCE BV, 2010)A history of deformation has been determined for the Cameli Basin located in the western part of the major Fethiye-Burdur Fault Zone, interpreted as the on-land continuation of Pliny-Strabo fault system (e.g., eastern ... -
Late Cenozoic stress state distributions at the intersection of the Hellenic and Cyprus Arcs, SW Turkey
Over, Semir; Ozden, Suha; Pinar, Ali; Yilmaz, Huseyin; Kamaci, Zuheyr; Unlugenc, Ulvi Can (PERGAMON-ELSEVIER SCIENCE LTD, 2016)The history of the Late Cenozoic stress regime was determined for an area between the gulfs of Fethiye and Antalya. Fault kinematic analysis and inversion of focal mechanisms of shallow earthquakes reveal significant ... -
Plio-Quaternary stress regime in Esen Cay Basin, SW Turkey
Over, Semir; Ozden, Suha; Yilmaz, Huseyin; Pinar, Ali; Unlugenc, Ulvi Can; Kamaci, Zuheyr (GEOLOGICAL SOC PUBLISHING HOUSE, 2013)The Plio-Quaternary Esen Cay Basin is situated at the junction of Hellenic and Cyprus arcs in southwestern Turkey. The basin is important for understanding the tectonic evolution of the region in relation to the Hellenic ... -
Plio-Quaternary Stress State in the Burdur Basin, SW-Turkey
Over, Semir; Yilmaz, Huseyin; Pinar, Ali; Ozden, Suha; Unlugenc, Ulvi Can; Kamaci, Zuheyr (ELSEVIER SCIENCE BV, 2013)This study defines the Plio-Quaternary to present day stress regime in the Burdur Basin, located at the northeastern end of the Fethiye-Burdur Fault Zone in SW Turkey. This fault length, which is considered the landward ... -
Upper crust response to geodynamic processes beneath Isparta Angle, SW Turkey: Revealed by CMT solutions of earthquakes
Over, Semir; Ozden, Suha; Kamaci, Zuheyr; Yilmaz, Huseyin; Unlugenc, Ulvi Can; Pinar, Ali (ELSEVIER SCIENCE BV, 2016)The Isparta Angle is an important area of SW Anatolia where extensions in all directions (N-S, NE-SW, NW-SE and E-W) meet These extensions were determined by normal faulting structures as well as by shallow earthquakes. ...