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
The Karakaya Complex: A Palaeotethyan Subduction/Accretion Complex from Northern Turkey
Date
2011-09-19
Author
Göncüoğlu, Mehmet Cemal
Sayıt, Kaan
Metadata
Show full item record
This work is licensed under a
Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License
.
Item Usage Stats
28
views
0
downloads
Cite This
URI
https://hdl.handle.net/11511/97989
Conference Name
Geoitalia 2011
Collections
Department of Geological Engineering, Conference / Seminar
Suggestions
OpenMETU
Core
The Cele mafic complex: Evidence for Triassic collision between the Sakarya and Istanbul Zones, NW Turkey
Bozkurt, Erdin; Satir, Muharrem (2013-06-04)
The lowest structural levels of the Istanbul Zone are exposed in the Sunnice Massif, north of Bolu. They comprise the greenschist-facies Ediacaran calc-alkaline bimodal Yellice metavolcanics, which are intruded by the Dirgine granitoid. Amphibolite-facies mafic and subordinate ultramafic rocks of the Cele mafic complex, hitherto termed the Cele meta-ophiolite, include hornblende gneisses of island arc meta-tholeiitic and transitional to calc-alkaline metagabbroic compositions, and were previously thought to...
The Karakoc magmatic association (central Anatolia, Turkey): Intrusive products of H2O and CO2 rich alkaline melt
KÖKSAL, FATMA; Göncüoğlu, Mehmet Cemal (2010-06-01)
The Karakoç magmatic association (central Anatolia, Turkey): Intrusive products of H2O and CO2 rich alkaline melt
Toksoy Köksal, Fatma (2010-06-13)
The Almacik mafic-ultramafic complex: exhumed Sakarya subcrustal mantle adjacent to the Istanbul Zone, NW Turkey
Bozkurt, Erdin; Satir, Muharrem; Crowley, Quentin G.; Ottley, Christian J. (2013-03-01)
The Almacik Mountains in northwestern Turkey expose an upper-amphibolite-facies complex consisting of alternating ultramafic (harzburgitic and websteritic) and mafic (metagabbroic) rock types. In the eastern part of this complex are island arc meta-tholeiites and transitional to calc-alkaline metabasites that are chemically quite similar to those of the Permo-Triassic Cele mafic complex north of Bolu, and this suggests an equivalence. However, much of the section exposes structurally deeper and chemically d...
The Palu-Uluova Strike-Slip Basin in the East Anatolian Fault System, Turkey: Its Transition from the Palaeotectonic to Neotectonic Stage
Colak, Serap; AKSOY, ERCAN; Kocyigit, Ali; İNCEÖZ, MURAT (2012-07-01)
The East Anatolian fault system (EAFS) is the 80-km-wide, 700-km-long, NE-trending sinistral strike-slip fault system forming a seismically very active intracontinental transfom fault boundary. It is located between Karhova County in the northeast and Karatas-Samandag counties in the southwest, and forms the southeastern boundary of the Anatolian platelet. The Palu-Uluova basin is one of several strike-slip basins located along the EAFS. It is surrounded by several push-ups such as the Karaomerdagi, Mastard...
Citation Formats
IEEE
ACM
APA
CHICAGO
MLA
BibTeX
M. C. Göncüoğlu and K. Sayıt, “The Karakaya Complex: A Palaeotethyan Subduction/Accretion Complex from Northern Turkey,” presented at the Geoitalia 2011, Turin, İtalya, 2011, Accessed: 00, 2022. [Online]. Available: https://hdl.handle.net/11511/97989.