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
Relict Seamounts within the Palaeotethyan Karakaya Complex, Turkey
Date
2009-12-14
Author
Sayıt, Kaan
Göncüoğlu, Mehmet Cemal
Furman, T
Metadata
Show full item record
This work is licensed under a
Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License
.
Item Usage Stats
102
views
0
downloads
Cite This
URI
https://hdl.handle.net/11511/98008
Conference Name
AGU
Collections
Department of Geological Engineering, Conference / Seminar
Suggestions
OpenMETU
Core
NEOGENE-RECENT SEDIMENTATION AND DEVELOPMENT OF THE ADANACILICIAN BASIN
EVANS, G; GORUR, N; ALAVI, N (1988-08-01)
The Adana-Cilician basin formed by interaction between the African, Arabian, and Anatolian plates. The basin has been filled asymmetrically from the north and northeast with the northeastern extremity having been completely filled to form the Adana basin beneath the plain of the Seyhan delta. There is no direct borehole evidence from the submarine areas, but coastal boreholes have revealed the presence of at least 6 km of Neogene sediment. The Burdigalian-Serravalian interval is dominated by turbidites and ...
Metamorphism in the Palaeozoic schists of the Southern Menderes Massif field petrographic textural and fabric data from Selimiye Milas Muğla area
Bozkurt, Erdin (1996-01-01)
Abstract: The Menderes Massif is a large-scale metamophic core-complex in western Anatolia and forms the western of two large metamorphic culminations in the Turkish Alpide orogen. Within the Southern Menderes Massif on the southern side of the Beßparmak Mountain north of Selimiye (Milas-MuÛla), two distinct lithologic groups are recognized on the basis of their lithology and structural position: the late Oligocene granitoid rocks now in the form of mylonitic augen gneiss and the structurally overlying sequ...
Dinoflagellate cyst biostratigraphy of Miocene strata in the Adana Basin, Eastern Mediterranean, Turkey
Turkecan, Aksel Tugba; Munsterman, Dirk; Isik, Ugras; Altıner, Demir; Pinar, Mehtap; Cevik, Tugba; Alay, Zeynep (Informa UK Limited, 2018-01-01)
The Adana Basin is one of the major Neogene basins situated in SW Turkey with sedimentary successions providing good records of the paleoenvironmental changes that affected the Mediterranean area. Since a detailed biochronostratigraphic framework has not been properly established in the Adana Basin yet, this study will be the first multidisciplinary approach carried out in this region. In addition, a detailed biozonation based on marine palynomorphs was the first ever documented from the Kopekli Formation d...
Fault trenching and geologic slip rates of the Húsavík-Flatey Fault, North Iceland
Harrington, John; Avşar, Ulaş; Klinger, Yann; Jonsson, Sigurjon; Gudmundsdottir, Esther (null; 2016-05-31)
Neotectonic characteristics and seismicity of the Dombayova Graben
Özacar, A. Arda; Koçyiğit, Ali; Department of Geological Engineering (2001)
Citation Formats
IEEE
ACM
APA
CHICAGO
MLA
BibTeX
K. Sayıt, M. C. Göncüoğlu, and T. Furman, “Relict Seamounts within the Palaeotethyan Karakaya Complex, Turkey,” presented at the AGU, California, Amerika Birleşik Devletleri, 2009, Accessed: 00, 2022. [Online]. Available: https://hdl.handle.net/11511/98008.