Show/Hide Menu
Hide/Show Apps
anonymousUser
Logout
Türkçe
Türkçe
Search
Search
Login
Login
OpenMETU
OpenMETU
About
About
Open Science Policy
Open Science Policy
Communities & Collections
Communities & Collections
Help
Help
Frequently Asked Questions
Frequently Asked Questions
Videos
Videos
Thesis submission
Thesis submission
Publication submission with DOI
Publication submission with DOI
Publication submission
Publication submission
Contact us
Contact us
Late Cretaceous to Recent kinematics of SE Anatolia (Turkey)
Date
2010-01-01
Author
Kaymakcı, Nuretdin
İNCEÖZ, MURAT
Ertepinar, P.
KOÇ, AYTEN
Metadata
Show full item record
This work is licensed under a
Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License
.
Item Usage Stats
6
views
0
downloads
Cite This
Five different deformation phases have been recognized in the SE Anatolian orogen and the Arabian Platform based on palaeostress inversion studies using fault-slip data sets. The timing and duration of these phases are determined using various criteria including the age of the affected strata, syndepositional structures, cross-cutting structures and overprinting slickensides. The oldest deformation phase is characterized generally by NE-SW-directed extension. The extension is thought to have resulted from slab-roll back processes during the Maastrichtian to Middle Eocene interval (c. 60 Ma to 40-35 Ma). The second deformation phase is characterized by east-west to NW-SE-directed compression and thought to result from cessation of roll-back processes possibly due to subduction of younger oceanic crust or increase in the convergence rate between Africa and Eurasia during the post-Middle Eocene to Late Oligocene interval (c. 40-35 Ma to 25 Ma). The third deformation phase is characterized by east-west to NW-SE-directed extension possibly due to slab detachment that initiated in Iran and migrated westwards during the latest Oligocene to Middle Miocene period (25-11 Ma). The fourth deformation phase is characterized by approximately north-south-directed compression due to collision and further northwards indentation of Arabian Plate by the end of Middle Miocene (11-3.5 Ma). The fifth and present deformation phase is characterized by NE-SW compression which might result from tectonic re-organization in the region since the Middle Pliocene (c. 3.5 Ma to recent).
Subject Keywords
Black-sea
,
Sedimentary basins
,
Neogene evolution
,
Malatya basin
,
Subduction
,
History
,
Western
,
Arc
,
Deformation
,
Lithosphere
URI
https://hdl.handle.net/11511/38290
Journal
SEDIMENTARY BASIN TECTONICS FROM THE BLACK SEA AND CAUCASUS TO THE ARABIAN PLATFORM
DOI
https://doi.org/10.1144/sp340.18
Collections
Department of Geological Engineering, Article
Citation Formats
IEEE
ACM
APA
CHICAGO
MLA
BibTeX
N. Kaymakcı, M. İNCEÖZ, P. Ertepinar, and A. KOÇ, “Late Cretaceous to Recent kinematics of SE Anatolia (Turkey),”
SEDIMENTARY BASIN TECTONICS FROM THE BLACK SEA AND CAUCASUS TO THE ARABIAN PLATFORM
, vol. 340, pp. 409–435, 2010, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/38290.