Eocene volcanism in the Central Anatolian Crystalline Complex: Geochemical indications for a change from post-collision to extension

Date

2008-07-01

Author

Göncüoğlu, Mehmet Cemal

Metadata

Show full item record

This work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.

Item Usage Stats

155
views

0
downloads

URI

https://hdl.handle.net/11511/55387

Collections

Graduate School of Natural and Applied Sciences, Conference / Seminar

Suggestions

OpenMETU
Core

Eocene post collisional volcanism in the Central Anatolian Crystalline Complex Turkey Petrology and geodynamic significance Geneli, Fatma; Göncüoğlu, Mehmet Cemal; Lassıter, J; Toksoy Köksal, Fatma (null; 2010-09-04) In the Central Anatolian Crystalline Complex (CACC) the Late Cretaceous postcollisional granitic magmatism is followed by Eocene extension, resulting in formation of roughly E-W trending transtensional basins. The volcanic rocks, mainly submarine lava flows and subareal domes are concentrated along these Middle Eocene (Bartonian) basins. The volcanic rocks are basic to intermediate and are classified as basalt, basaltic andesite and rarely alkali basalt and trachy-andesite. Petrographically they are general...
Conodont biostratigraphy and depositional environments of the uppermost visean-lower serpukhovian units from the central taurides (Bademli Region) Özdemir,özdemir, Ayşe,ayşe; Altıner, Demir; Altıner, Sevinç (null; 2018-09-03) The sections (BS and BSE) cropping out in the Bademli region (Turkey) have been studied in order to define distinct microfacies types and associated depositional environments and the conodont biostratigraphy of the carbonate units. Conodonts are one of the main microfossil groups used to date and correlate the Paleozoic rocks. Several beds within the measured sections in Taurides are barren of conodonts, while others contain not very abundant, but quite important taxa. Based on the appearance of biostratigr...
Plio-quaternary sediments,paleo-topography of the messinian evaporities,and salt tectonism in the Cilicia Basin,Northeastern Mediterranean Sea Toker, Mustafa; Ediger, Vedat; Department of Marine Geology and Geophysics (2003)
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 ...
Proterozoic ophiolites and mafic-ultramafic complexes marginal to the Istanbul Block: An exotic terrane of Avalonian affinity in NW Turkey Bozkurt, Erdin; YİĞİTBAŞ, ERDİNÇ; Ottley, Christopher J. (Elsevier BV, 2008-12-01) Among the Proterozoic inliers in the Istanbul Block, the lowest structural levels are exposed in the Sunnice Massif, north of Bolu. Amphibolite-facies mafic and subordinate ultramafic rocks of the Cele meta-ophiolite underlie the greenschist-facies Ediacaran calc-alkaline Yellice metavolcanics, which are intruded by the similar to 565-576 Ma Dirgine granitoids. Homblende gneisses of the Cele meta-ophiolite comprise island arc metatholeiites and transitional to calc-alkaline metabasalts which, together with ...

Citation Formats

M. C. Göncüoğlu, “Eocene volcanism in the Central Anatolian Crystalline Complex: Geochemical indications for a change from post-collision to extension,” 2008, vol. 72, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/55387.