Neotectonics of Turkey–a synthesis

E Bozkurt - Geodinamica acta, 2001 - Taylor & Francis
Turkey forms one of the most actively deforming regions in the world and has a long history
of devastating earthquakes. The belter understanding of its neotectonic features and active …

The spread of grass-dominated habitats in Turkey and surrounding areas during the Cenozoic: phytolith evidence

CAE Strömberg, L Werdelin, EM Friis… - Palaeogeography …, 2007 - Elsevier
The arrival of hipparionine horses in the eastern Mediterranean region around 11 Ma was
traditionally thought to mark the simultaneous westward expansion of savanna vegetation …

Petrology and geochemistry of post-collisional Middle Eocene volcanic units in North-Central Turkey: evidence for magma generation by slab breakoff following the …

M Keskin, ŞC Genç, O Tüysüz - Lithos, 2008 - Elsevier
The Eocene volcano-sedimentary units of Northern Anatolia are confined into a narrow zone
trending parallel to the Intra Pontide and İzmir–Ankara–Erzincan sutures, along which the …

Kinematic development and paleostress analysis of the Denizli Basin (Western Turkey): implications of spatial variation of relative paleostress magnitudes and …

N Kaymakci - Journal of Asian Earth Sciences, 2006 - Elsevier
Paleostress orientations and relative paleostress magnitudes (stress ratios), determined by
using the reduced stress concept, are used to improve the understanding of the kinematic …

Seismotectonic database of Turkey

TY Duman, T Çan, Ö Emre, FT Kadirioğlu… - Bulletin of Earthquake …, 2018 - Springer
Turkey is located in one of the most seismically active regions in the world. Characterizing
seismic source zones in this region requires evaluation and integration of geological …

[LIBRO][B] Tectono-stratigraphy of the Çankırı Basin: late Cretaceous to early Miocene evolution of the Neotethyan suture zone in Turkey

N Kaymakci, Y Özçelik, SH White, PM Van Dijk - 2009 - lyellcollection.org
The Çankırı Basin straddles the İzmir–Ankara–Erzincan Suture Zone which demarcates the
former position of the northern branch of the Neotethys. It includes more than 3 km of pre …

Late Cretaceous to Paleocene oroclinal bending in the central Pontides (Turkey)

MJM Meijers, N Kaymakci, DJJ Van Hinsbergen… - …, 2010 - Wiley Online Library
The Turkish Pontide fold‐and‐thrust belt formed since the Paleozoic and is an important
element in the Africa‐Eurasia convergence and the resulting closure of the Neo‐Tethys …

3-D crustal structure along the North Anatolian Fault Zone in north-central Anatolia revealed by local earthquake tomography

S Yolsal-Cevikbilen, CB Biryol, S Beck… - Geophysical Journal …, 2012 - academic.oup.com
DP-wave velocity structure and Vp/Vs variations in the crust along the North Anatolian Fault
Zone (NAFZ) in north-central Anatolia were investigated by the inversion of local P-and S …

Dating of the Black Sea Basin: new nannoplankton ages from its inverted margin in the Central Pontides (Turkey)

JC Hippolyte, C Müller, N Kaymakci… - … Society, London, Special …, 2010 - lyellcollection.org
The Eocene uplift and inversion of a part of the Black Sea margin in the Central Pontides,
allows us to study the stratigraphic sequence of the Western Black Sea Basin (WBS). The …

Neotethyan Ankara Melange, central Turkey in its Triassic-Eocene regional tectonic setting including accretionary melanges, magmatic arcs and continental units

A Harry Forbes Robertson, O Parlak… - International Geology …, 2023 - Taylor & Francis
ABSTRACT The classic Neotethyan Ankara Melange formed within the Triassic-Eocene
İzmir-Ankara-Erzincan ocean ('N Neotethys'), bordered in central Anatolia by the Kırşehir …