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
Cross-sectional anatomy and geodynamic evolution of the Central Pontide orogenic belt (northern Turkey)
Download
index.pdf
Date
2016-01-01
Author
Hippolyte, JC
Espurt, Nikolas
Kaymakcı, Nuretdin
SANĞU, ERCAN
Mueller, C.
Metadata
Show full item record
This work is licensed under a
Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License
.
Item Usage Stats
182
views
365
downloads
Cite This
Geophysical data allowed the construction of a similar to 250-km-long lithospheric-scale balanced cross section of the southern Black Sea margin (Espurt et al. in Lithosphere 6:26-34, 2014). In this paper, we combine structural field data, stratigraphic data, and fault kinematics analyses with the 70-km-long onshore part of the section to reconstruct the geodynamic evolution of the Central Pontide orogen. These data reveal new aspects of the structural evolution of the Pontides since the Early Cretaceous. The Central Pontides is a doubly vergent orogenic wedge that results from the inversion of normal faults. Extensional subsidence occurred with an ENE-trend from Aptian to Paleocene. We infer that the Black Sea back-arc basin also opened during this period, which was also the period of subduction of the Tethys Ocean below the Pontides. As in the Western Pontides, the Cretaceous-Paleocene subsidence was interrupted from Latest Albian to Coniacian time by uplift and erosion that was probably related to a block collision and accretion in the subduction zone. The restoration of the section to its pre-shortening state (Paleocene) shows that fault-related subsidence locally reached 3600 m within the forearc basin. Structural inversion occurred from Early Eocene to Mid-Miocene as a result of collision and indentation of the Pontides by the KA +/- rAYehir continental block to the south, with 27.5 km (similar to 28 %) shortening along the section studied. The inversion was characterized by NNE-trending shortening that predated the Late Neogene dextral escape of Anatolia along the North Anatolian Fault and the modern stress field characterized by NW-trending compression within the Eocene Boyabat basin.
Subject Keywords
Pontides
,
Black Sea
,
North Anatolian fault
,
Cross section
,
Paleostress
,
Geodynamics
URI
https://hdl.handle.net/11511/43118
Journal
INTERNATIONAL JOURNAL OF EARTH SCIENCES
DOI
https://doi.org/10.1007/s00531-015-1170-6
Collections
Department of Geological Engineering, Article
Suggestions
OpenMETU
Core
Stratigraphic comparisons along the Pontides (Turkey) based on new nannoplankton age determinations in the Eastern Pontides: geodynamic implications
Hippolyte, JC; Muller, C.; Sangu, Ercan; Kaymakcı, Nuretdin (2017-01-01)
We compared the stratigraphic formations along the southern margin of the Black Sea using 196 nannoplankton ages determined in the Western and Central Pontides and 112 new samples from the Eastern Pontides. We inferred that the I. stanbul and Sakarya zones were amalgamated prior to the Early Cretaceous. Extensional subsidence migrated eastwards along the Pontides from the Barremian to the Paleocene. The eastwards younging of the Cretaceous magmatism suggested that the eastern Black Sea Basin is younger. Loc...
Possible sources and mechanisms of manganese enrichment in the deep-sea sedıments of the Marmara trough depressions (ne-Mediterranean, Turkey)
ERGIN, M (1994-01-01)
Enrichment of Mn in deep-water relative to shallow-water sediments in the Marmara Basin was investigated using earlier metal data and some geochemical information from other similar marine regions on a comparative basis. Deep-water (1152-1276 m) sediments from the three depressions located along the Marmara Trough of the seismically-active North Anatolian Fault Zone contained much higher Mn concentrations (< 6355 ppm; over 10 600 ppm in some core horizons; on a carbonate-free basis) than those from the surr...
Fluids along the North Anatolian Fault, Niksar basin, north central Turkey: Insight from stable isotopic and geochemical analysis of calcite veins
Sturrock, Colin P.; Catlos, Elizabeth J.; Miller, Nathan R.; AKGÜN, AYKUT; Fall, Andras; Gabitov, Rinat I.; Yılmaz, İsmail Ömer; Larson, Toti; Black, Karen N. (2017-08-01)
Six limestone assemblages along the North Anatolian Fault (NAF) Niksar pull-apart basin in northern Turkey were analyzed for delta O-18(PDB) and delta C-13(PDB) using bulk isotope ratio mass spectrometry (IRMS). Matrix vein differences in delta O-18(PDB) (-2.1 to 6.3 parts per thousand) and delta C-13(PDB) (-0.9 to 4.6 parts per thousand) suggest a closed fluid system and rock buffering. Veins in one travertine and two limestone assemblages were further subjected to cathodoluminescence, trace element (Laser...
Helium isotope variations in Turkey: relationship to tectonics, volcanism and recent seismic activities
Güleç, Nilgün Türkan; Mutlu, H (2002-07-01)
The distribution of helium isotope ratios in the various tectonic provinces of Turkey is examined through a synthesis of previously published data and the results of a recent survey along the North Anatolian Fault Zone (NAFZ) following the catastrophic 1999 earthquakes. The R/R-A values (where R = sample He-3/He-4 and RA = air He-3/He-4) cover a wide range from 0.05 to 7.87, and the mantle-derived helium is clearly identified in most locations, The mantle-derived component is high (> 50% of total He) in (a)...
Identification of morphometric properties of basins located on western part of NAFZ
Sarp, Gülcan; Toprak, Vedat; Düzgün, H. Şebnem; Department of Geodetic and Geographical Information Technologies (2012)
This study aims to investigate tectonic activity levels and development stages of the tectonic and hydrologic basin areas located on western part of the main trace of the North Anatolian Fault Zone (NAFZ) using quantitative measurement techniques. The basins investigated are Bolu, Yeniçağa, Dörtdivan, Çerkes, Ilgaz and Tosya. The methodology includes application of six morphometric indices (Basin Shape, Hypsometric curve and Hypsometric Integral, Sinuosity of Mountain Fronts, Stream Length Gradient Index, V...
Citation Formats
IEEE
ACM
APA
CHICAGO
MLA
BibTeX
J. Hippolyte, N. Espurt, N. Kaymakcı, E. SANĞU, and C. Mueller, “Cross-sectional anatomy and geodynamic evolution of the Central Pontide orogenic belt (northern Turkey),”
INTERNATIONAL JOURNAL OF EARTH SCIENCES
, pp. 81–106, 2016, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/43118.