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The Tarakli Flysch in the Boyali area (Sakarya Terrane, northern Turkey): Implications for the tectonic history of the IntraPontide suture zone
Date
2013-11-01
Author
Catanzariti, Rita
Ellero, Alessandro
Göncüoğlu, Mehmet Cemal
Marroni, Michele
Ottria, Giuseppe
Pandolfi, Luca
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In the Boyali area, northern Turkey, the tectonic units of the Istanbul-Zonguldak Terrane and the IntraPontide suture zone are thrust over the deposits at the top of the Sakarya Terrane, known as Tarakli Flysch. It consists of Early Maastrichtian-Middle Paleocene turbidite and mass-gravity deposits, whose source mainly corresponds to the Istanbul-Zonguldak Terrane, and, with a lesser extent, to the IntraPontide suture zone. These deposits were sedimented in a foredeep basin developed during the convergence between Sakarya and Eurasian continental microplates. In the Late Paleocene-Early Eocene time span, the Tarakli Flysch was deformed (D1 phase) during the closure of the foredeep basin. In the Miocene time, the strike-slip tectonics (D2 phase) related to the North-Anatolian fault produced further deformations of the Tarakli Flysch. (C) 2013 Academie des sciences. Published by Elsevier Masson SAS. All rights reserved.
Subject Keywords
Foredeep deposits
,
Sakarya Terrane
,
IntraPontide suture zone
,
Tarakli Flysch
,
Northern Turkey
URI
https://hdl.handle.net/11511/32394
Journal
COMPTES RENDUS GEOSCIENCE
DOI
https://doi.org/10.1016/j.crte.2013.11.001
Collections
Graduate School of Natural and Applied Sciences, Article
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R. Catanzariti, A. Ellero, M. C. Göncüoğlu, M. Marroni, G. Ottria, and L. Pandolfi, “The Tarakli Flysch in the Boyali area (Sakarya Terrane, northern Turkey): Implications for the tectonic history of the IntraPontide suture zone,”
COMPTES RENDUS GEOSCIENCE
, pp. 454–461, 2013, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/32394.