Show/Hide Menu
Hide/Show Apps
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
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
MANTLE SOURCE REGION AND PARTIAL MELTING CONDITIONS OF THE PLIOCENE VOLCANISM IN THE EAST ANATOLIA COLLISION ZONE, TURKEY
Date
2018-05-11
Author
Özdemir, Yavuz
Oyan, Vural
Keskin, Mehmet
Güleç, Nilgün Türkan
Metadata
Show full item record
Item Usage Stats
98
views
0
downloads
Cite This
URI
https://hdl.handle.net/11511/73361
Collections
Unverified, Conference / Seminar
Suggestions
OpenMETU
Core
Sedimentary cyclicity and micropaleontological investigations in the upper triassic shallow marine carbonate successions (central and western taurides, turkey)
Coşkun Tunaboylu, Burcu; Altıner, Demir; Department of Geological Engineering (2008)
Shallowing-upward meter-scale cycles (parasequences) consisting of megalodont-bearing limestones or clay levels at the bottom and fenestral limestones, breccias, stromatolites or vadose pisoids at the top constitute the basic working units of the Upper Triassic successions in the Central and Western Taurides. These cycles are mainly represented by subtidal through supratidal carbonate facies and known as Lofer cycles in the literature. The presence of breccias, mud cracks, dissolution vugs and vadose pisoid...
Sedimentary geochemical evidence of historical tsunamis in the Eastern Mediterranean from oludeniz Lagoon, SW Turkey
Avşar, Ulaş (2019-03-01)
In the Eastern Mediterranean and southern Aegean seas, historical records indicate there were 17 tsunamis in the last 2500years with intensities>6 on a 12-point tsunami intensity scale. Regional geologic records of past tsunamis, however, are not sufficiently well-documented to assess tsunami hazards. This study presents geochemical evidence of historic tsunamis in the Eastern Mediterranean for the last 700years, detected in the sedimentary sequence of oludeniz Lagoon, SW Turkey. Sediment chronology was est...
Mantle Convection beneath the Aegir Ridge, a Shadow in the Iceland Hotspot
Sayıt, Kaan; Howell, S.M.; Ito, G.; Breivik, A.J.; Hanan, B.B.; Vogt, P.R.; Mjelde, R.; Pedersen, R.B. (2012-12-03)
Sedimentary cyclicity in the upper cretaceous successions of the Haymana Basin (Turkey): depositional sequences as response to relative sea level changes
Huseynov, Afgan; Altıner, Demir; Department of Geological Engineering (2007)
The Haymana basin in Central Anatolia (Turkey) formed on a Late Cretaceous to Middle Eocene fore arc accretionary wedge. The aim of this study is to investigate the sedimentary cyclicity and depositional sequences in the Upper Cretaceous clastic successions of the Haymana basin. To be able to achieve this objective, a 250 m stratigraphic section, which is mainly composed of siliciclastics has been measured in the Haymana Basin. In this study, detailed lithofacies analyses were performed and five different ...
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
Y. Özdemir, V. Oyan, M. Keskin, and N. T. Güleç, “MANTLE SOURCE REGION AND PARTIAL MELTING CONDITIONS OF THE PLIOCENE VOLCANISM IN THE EAST ANATOLIA COLLISION ZONE, TURKEY,” 2018, vol. 9, Accessed: 00, 2021. [Online]. Available: https://hdl.handle.net/11511/73361.