T184 The Dynamics of Tectono-Sedimentary Systems During Basin Formation and Fill (Posters)
Monday, 23 October 2017
9:00 AM - 6:30 PM
Halls 4EF
CHRONOLOGY OF SUTURING AND POST-COLLISIONAL DEFORMATION OF THE ANATOLIAN OROGENY, TURKEY: INSIGHTS FROM GEOCHRONOLOGY AND SEDIMENTOLOGY OF THE SARICAKAYA BASIN, WESTERN ANATOLIA
Paper number: T184-6
Program: Technical Sessions
Time: 9:00 AM – 6:30 PM
Authors
-
Alexis LichtUniversity of Washington, Seattle, WA
-
Clay CampbellUniversity of Kansas, Lawrence, KS
-
Faruk OcakoğluEskişehir Osmangazi University, Eskişehir
-
Michael TaylorUniversity of Kansas, Lawrence, KS
-
Lauren BurchUniversity of Washington, Seattle, WA
-
Pauline CosterUniversity of Kansas, Lawrence, KS
-
Grégoire MétaisMuséum National d'Histoire Naturelle, Paris
-
K. Christopher BeardUniversity of Kansas, Lawrence, KS
Abstract
Here, we investigate the timing and dynamics of suturing and deformation in the Saricakaya Basin, a 100 km long basin on the Pontides developed along the Izmir-Ankara-Erzincan suture zone. The Saricakaya basin exposes a thick, Paleocene(?)-Eocene sedimentary sequence thrusted by post-collisional orogenic build-up, making this basin an ideal location to determine the chronology of collision and early fold and thrust belt development. New age constraints from U/Pb dating of volcanic deposits, and new data from U/Pb detrital zircon geochronology, sandstone petrology and sedimentary facies reveal changes in provenance and depositional environments related to the post-collisional evolution of the suture zone. These results improve understanding of how the Anatolian orogeny evolved through time and provide key constraints to investigate how regional geodynamics influenced Middle Eastern biogeography.
Geological Society of America Abstracts with Programs. Vol. 49, No. 6
doi: 10.1130/abs/2017AM-299600
© Copyright 2017 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.