Show/Hide Menu
Hide/Show Apps
Logout
Türkçe
Türkçe
Search
Search
Login
Login
OpenMETU
OpenMETU
About
About
Open Science Policy
Open Science Policy
Open Access Guideline
Open Access Guideline
Postgraduate Thesis Guideline
Postgraduate Thesis Guideline
Communities & Collections
Communities & Collections
Help
Help
Frequently Asked Questions
Frequently Asked Questions
Guides
Guides
Thesis submission
Thesis submission
MS without thesis term project submission
MS without thesis term project submission
Publication submission with DOI
Publication submission with DOI
Publication submission
Publication submission
Supporting Information
Supporting Information
General Information
General Information
Copyright, Embargo and License
Copyright, Embargo and License
Contact us
Contact us
Strike-slip neotectonic regime and related structures in the Cappadocia region: a case study in the Salanda basin, Central Anatolia, Turkey
Download
index.pdf
Date
2016-01-01
Author
Kocyigit, Ali
DOĞAN, UĞUR
Metadata
Show full item record
This work is licensed under a
Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License
.
Item Usage Stats
228
views
0
downloads
Cite This
The study area is a strike-slip basin of approximately 1-9 km wide, 66 km long and N65 degrees W trending, located between the historical Kesikkopru in the west and the Sarihidir settlement in the east along the northern side of the Central Anatolian Volcanic Province. It was evolved on a regional erosional surface of a pre-Quaternary volcanosedimentary sequence during Quaternary. This is evidenced by the stratigraphical, structural, and seismic data. The total amounts of throw and dextral strike-slip displacement accumulated on the basin-boundary faults during the evolutionary history of the basin are 178 m and 5 km, respectively. The average slip rate on the Salanda master fault is approximately 4 mm/year since the late early Pleistocene based on the total dextral strike-slip offset accumulated on it. The throw amount is small compared with the dextral strike-slip offset, which implies a strike-slip regime rather than a tensional tectonic regime in the basin. This is also supported by the combination of both the contractional and extensional structures such as reverse faults, fissure-ridge travertines, and a series of stepped terraces of late Quaternary age. Finally, it would be useful to take this paper into account in new works to be carried out in other sections of the Cappadocia region, because a new neotectonic regime (strike-slip tectonic regime) is first introduced here for this region.
Subject Keywords
Central Anatolian Volcanic Province
,
Quaternary
,
Kizilirmak River
,
Strike-slip neotectonic regime
,
Cappadocia
,
Salanda basin
URI
https://hdl.handle.net/11511/64445
Journal
TURKISH JOURNAL OF EARTH SCIENCES
DOI
https://doi.org/10.3906/yer-1512-9
Collections
Department of Geological Engineering, Article
Suggestions
OpenMETU
Core
TECTONIC CONTROL ON THE DEVELOPMENT OF THE NEOGENE QUATERNARY CENTRAL ANATOLIAN VOLCANIC PROVINCE, TURKEY
TOPRAK, V; Göncüoğlu, Mehmet Cemal (1993-12-01)
The Neogene-Quaternary Central Anatolian Volcanic Province (CAVP) is elongated in a north-east south-west direction within pre-Oligocene basement in central Turkey. This study investigates the field evidence relating to the development of the CAVP.
Noble gases and rock geochemistry of alkaline intraplate volcanics from the Amik and Ceyhan-Osmaniye areas, SE Turkey
Italiano, F.; YÜCE, GALİP; Di Bella, M.; Rojay, Fuat Bora; Sabatino, G.; Tripodo, A.; Martelli, M.; Rizzo, A. L.; Misseri, M. (2017-10-10)
The SE part of Turkey is characterized by a transtensional regime within the complex collision zone between the Anatolian, Arabian and African plates, which is bounded by two main faults, Dead Sea Fault and its splays on east and the Karasu Fault on west. In this tectonic and geodynamic context developed the Amik and further North, Erzin and Toprakkale districts, which are located onshore the Iskenderun Gulf, with the occurrence of a widespread and young alkaline volcanism dated from 1.57 to 0.05 Ma in Amik...
Sedimentary records of past earthquakes in Boraboy Lake during the last ca 600 years (North Anatolian Fault, Turkey)
Avşar, Ulaş; De Batıst, Marc; Schmidt, Sabine; Fagel, Nathalie (2015-09-01)
Multiproxy sedimentological analyses along 4.9 m-long sequence of Boraboy Lake, which is located on the central eastern part of the North Anatolian Fault (NAF), reveal the sedimentary traces of past large earthquakes in the region. The lake has a relatively large catchment area (10 km(2)) compared to its size (0.12 km(2)), which renders sedimentation sensitive to heavy rain/storm events. Accordingly, the background sedimentation, which is composed of faintly laminated reddish/yellowish brown clayey silt, is...
Heat flow in the Sea of Marmara Central Basin: Possible implications for the tectonic evolution of the North Anatolian fault
Grall, Celine; Henry, Pierre; Tezcan, Devrim; de Lepinay, Bernard Mercier; Becel, Anne; Geli, Louis; Rudkiewicz, Jean-Luc; Zitter, Tiphaine; Harmegnies, Francois (2012-01-01)
The Central Basin in the Sea of Marmara is a syntectonic basin related to the evolution of the North Anatolian fault. A well-dated (ca. 15.5-16 ka) homogenite sediment can be used as a marker in three-dimensional depth model calculations, allowing a precise determination of the seafloor subsidence rates during the Holocene. A steady-state model based on the propagation of the rates downward through the basin fill provides a good correlation with the deeper seismic reflection imagery for the past 250 ka but ...
Oblique Deformation in Central Turkey: Fault Interaction and River Incision at the Intersection of the Tuz Gölü and Central Anatolian Fault Zones
Schoenbohm, Lindsay; Tokay, Bülent; Krystopowicz, Neil; Higgins, Mark; Rojay, Fuat Bora; Brocard, Gilles (null; 2014-12-15)
Although much of the deformation associated with Arabia-Eurasia collision and Aegean extension is expressed by westward translation of Central Anatolia along the North Anatolian and East Anatolian fault zones, important deformation also takes place in the interior. Major interior faults include the NE-SW striking, left-lateral Central Anatolian fault zone (CAFZ), which splays from the NAFZ, and the NW-SE striking, right-lateral Tuz Gölü fault zone (TGFZ). We examine fault kinematics and river incision in th...
Citation Formats
IEEE
ACM
APA
CHICAGO
MLA
BibTeX
A. Kocyigit and U. DOĞAN, “Strike-slip neotectonic regime and related structures in the Cappadocia region: a case study in the Salanda basin, Central Anatolia, Turkey,”
TURKISH JOURNAL OF EARTH SCIENCES
, pp. 393–417, 2016, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/64445.