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
Geology and petrology of the kösedağ metavolcanic rocks to the south of Tosya
Download
index.pdf
Date
2015
Author
Berber, Faruk
Metadata
Show full item record
Item Usage Stats
197
views
84
downloads
Cite This
The Kösedağ Metavolcanics crops out in the southern Central Pontides as a NE-SW trending belt to the south of Tosya. This unit is characterized by a low-grade metavolcanic assemblage interbedded with metasedimentary lithologies. While these metavolcanics are bounded to the north by the North Anatolian Fault Zone, they structurally overlie the metacarbonates of the Dikmen Formation in the south. Petrographically, the Kösedağ Metavolcanics are characterized by metadacites, metaandesites and metabasalts. The metadacites within this unit include abundant quartz phenocrysts, whereas the metaandesites are plagioclase-phyric. The metabasalts, on the other hand, consists of clinopyroxene and plagioclase as the dominant primary phases. All these metavolcanics have been influenced by low-grade metamorphism. In addition, the Kösedağ Metavolcanics appear to have been affected by mylonitic deformation along the NAFZ. The Kösedağ Metavolcanics are characterized by a wide range of chemical compositions including basalts, andesites and dacites. The Kösedağ Metavolcanics are subdivided into two groups as Type 1 and Type 2 based on trace element systematics. The Kösedağ Metavolcanics display enrichment in Th and LREE relative to HFSE, and characterized by negative Nb anomalies, suggesting involvement of subduction component. The high Zr/Nb, low Zr/Y and Nb/Y signatures of the Kösedağ Metavolcanics indicate that they have derived from a depleted mantle source similar to N-MORB source. Geochemical signatures of the Kösedağ Metavolcanics suggest that they have formed above a subduction zone. Considering also their geological characteristics, the Kösedağ Metavolcanics appear to represent remnants of an island arc within a Neotethyan branch during the Late Cretaceous.
Subject Keywords
Petrology.
,
Igneous rocks.
,
Physical geology.
,
Volcanic ash, tuff, etc.
URI
http://etd.lib.metu.edu.tr/upload/12619177/index.pdf
https://hdl.handle.net/11511/24976
Collections
Graduate School of Natural and Applied Sciences, Thesis
Suggestions
OpenMETU
Core
Geological, mineralogical and geochemical characteristics of Mississippian K-bentonites from southern Turkey: A correlation with coeval tephras from Gondwana-derived terranes
Bozkaya, Ömer; Günal Türkmenoğlu, Asuman; Göncüoğlu, Mehmet Cemal; Okuyucu, Cengiz (2021-09-01)
Five thin (5–15 cm) and yellowish green tephra (K-bentonite) layers are exposed along two sections in the south of Akşehir (Konya, southern Turkey) within the Early Carboniferous (Mississippian) red dolomite-dolomitic limestone succession of the Sultandağ Unit in the central Tauride Belt. K-bentonites exhibit typical porphyritic texture with euhedral plagioclase phenocrysts replaced by fine-grained white K-micas and sparry dolomite crystals. The intensively sericitized volcanic matrix has vitrophyric textur...
GEOCHEMISTRY AND PETROGENESIS OF THE ARC-RELATED KÖSDAĞ METAVOLCANICS, SOUTHERN CENTRAL PONTIDES, NORTHERN TURKEY
Berber, Faruk; Sayıt, Kaan; Department of Geological Engineering (2021-12-27)
The Kösdağ Metavolcanics (KM) in the southern Central Pontides crops out between the Izmir-Ankara-Erzincan Suture Zone (IAESZ) in the south and the Sakarya Composite Terrane in the north. The unit is represented by a low-grade metamorphic assemblage including meta-basics, meta-intermediates, and meta-felsics, interlayered with recrystallized limestone, mudstone, and chert. While the unit is bounded to the north by the North Anatolian Fault Zone (NAFZ), the Dikmen Formation stratigraphically overlie the unit...
Geological evolution of the gediz graben, sw turkey: temporal and spatial variation of the graben
Çiftçi, Bozkurt N; Bozkurt, Erdin; Department of Geological Engineering (2007)
Gediz Graben is a continental extensional basin filled with Neogene sediments. Its margins are controlled by active ~EW-trending fault systems with major system, in terms of total offset and duration of activity, located along the southern margin. The graben evolved as a half graben by the activity of the southern margin during the entire Miocene. Then, the northern margin-bounding structure initiated by PlioQuaternary to form the current configuration of the graben with an inherited asymmetry. The southern...
Geology and petrology of Beypazari Granitoids : Yassikaya sector
Billur, Başak; Lünel, A. Taylan; Department of Geological Engineering (2004)
Beypazari Granitoid is a low temperature and shallow-seated batholite intruded the Tepeköy metamorphic rocks of the Central Sakarya Terrane. Composition of the granitoid varies from granite to diorite. The granitoid is unconformably overlain by Palaeocene and Eocene rock units. Thus the age is probably Late Cretaceous. The Beypazari Granitoid comprises mafic microgranular enclaves. The granitoid mainly consists of quartz, plagioclase, orthoclase and minor amphibole, biotite, chlorite, zircon, sphene, apatit...
Surface expression of eastern Mediterranean slab dynamics: Neogene topographic and structural evolution of the southwest margin of the Central Anatolian Plateau, Turkey
Schildgen, T. F.; Cosentino, D.; Caruso, A.; Buchwaldt, R.; Yildirim, C.; Bowring, S. A.; Rojay, Fuat Bora; Echtler, H.; Strecker, M. R. (2012-03-16)
The southwest margin of the Central Anatolian Plateau has experienced multiple phases of topographic growth, including the formation of localized highs prior to the Late Miocene that were later affected by wholesale uplift of the plateau margin. Our new biostratigraphic data limit the age of uplifted marine sediments at the southwest plateau margin at 1.5 km elevation to <7.17 Ma, and regional lithostratigraphic correlations imply that the age is <6.7 Ma. Single-grain CA-TIMS U-Pb zircon analyses from a rew...
Citation Formats
IEEE
ACM
APA
CHICAGO
MLA
BibTeX
F. Berber, “Geology and petrology of the kösedağ metavolcanic rocks to the south of Tosya,” M.S. - Master of Science, Middle East Technical University, 2015.