Tectonic evolution of the Gediz Graben: field evidence for an episodic, two-stage extension in western Turkey
Western Turkey is one of the most spectacular regions of widespread active continental
extension in the world. The most prominent structures of this region are E–W-trending …
extension in the world. The most prominent structures of this region are E–W-trending …
A comprehensive classification of Earthquake Archaeological Effects (EAE) in archaeoseismology: Application to ancient remains of Roman and Mesoamerican …
MA Rodríguez-Pascua, R Pérez-López… - Quaternary …, 2011 - Elsevier
One of the key tasks in archaeoseismology is to test whether the recorded building damage
in ancient cities can be related to ancient earthquakes. Archaeologists often claim …
in ancient cities can be related to ancient earthquakes. Archaeologists often claim …
The Denizli graben-horst system and the eastern limit of western Anatolian continental extension: basin fill, structure, deformational mode, throw amount and episodic …
A Koçyiğit - Geodinamica Acta, 2005 - Taylor & Francis
The Denizli graben-horst system (DGHS) is located at the eastern-southeastern converging
tips of three well-identified major grabens, the Gediz, the Küçük Menderes and the Büyük …
tips of three well-identified major grabens, the Gediz, the Küçük Menderes and the Büyük …
Granitoid rocks of the southern Menderes Massif (southwestern Turkey): field evidence for Tertiary magmatism in an extensional shear zone
E Bozkurt - International Journal of Earth Sciences, 2004 - Springer
Recent field campaign in the southern Menderes Massif in southwestern Turkey revealed
that the so-called 'core of the massif'comprises two distinct types of granitoid rocks: an …
that the so-called 'core of the massif'comprises two distinct types of granitoid rocks: an …
[PDF][PDF] Introduction: Evolution of continental extensional tectonics of western Turkey
Turkey is located on the seismically active Mediterranean Earthquake Belt. The country is
one of the most actively deforming regions of the world and has a long history of devastating …
one of the most actively deforming regions of the world and has a long history of devastating …
Oligo-Miocene extension in the Lycian orogen: evidence from the Lycian molasse basin, SW Turkey
H Sözbilir - Geodinamica Acta, 2005 - Taylor & Francis
The Lycian molasse basin of SW Turkey is a NE-SW-oriented basin that developed on an
imbricated basement, comprising the allochthonous Mesozoic rocks of the Lycian nappes …
imbricated basement, comprising the allochthonous Mesozoic rocks of the Lycian nappes …
Determination of horizontal extension from fissure-ridge travertines: a case study from the Denizli Basin, southwestern Turkey
Travertine deposits reflect some aspects of the regional tectonics because of the close
association between travertine deposits and active fractures, that later of which provide …
association between travertine deposits and active fractures, that later of which provide …
Sea level change and vertical land movements since the last two millennia along the coasts of southwestern Turkey and Israel
This paper provides new relative sea level data inferred from coastal archaeological sites
located along the Turkish coasts of the Gulf of Fethye (8 sites), and Israel, between Akziv …
located along the Turkish coasts of the Gulf of Fethye (8 sites), and Israel, between Akziv …
Archaeoseismic record at the ancient Roman city of Baelo Claudia (Cádiz, south Spain)
This study represents the first paleoseismic approach in Spain in which archaeological
remains are considered. The ancient Roman city of Baelo Claudia (1st–4th centuries AD) …
remains are considered. The ancient Roman city of Baelo Claudia (1st–4th centuries AD) …
Evidence for two episodes of volcanism in the Bigadiç borate basin and tectonic implications for western Turkey
Evidence for two episodes of volcanism in the Bigadiç borate basin and tectonic implications for
western Turkey Page 1 GEOLOGICAL JOURNAL Geol. J. 40: 545–570 (2005) Published online …
western Turkey Page 1 GEOLOGICAL JOURNAL Geol. J. 40: 545–570 (2005) Published online …