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Different modes of stress transfer in a strike-slip fault zone: an example from the North Anatolian Fault System in Turkey
(Scientific Technical Research Council Turkey-Tubitak, 2007)
The dextral North Anatolian Fault System (NAFS) extends for well over 1000 km from the compressive tectonic domain of eastern Anatolia into the broad and diverse tectonic domain of the western Anatolian, Marmara and Aegean ...
Two-and-Three-Dimensional Crustal Thickness of the Eastern Pontides (NE Turkey)
(Scientific Technical Research Council Turkey-Tubitak, 2009)
The Eastern Pontide orogenic belt is divided into three subzones ( northern, southern and axial zones) based on present lithologies and facies associations. NE-SW-, NW-SE- and E-W-trending fault systems, which play an ...
Mid-cretaceous olistostromal ophiolitic melange developed in the back-are basin of the eastern Pontide magmatic arc, Northeast Turkey
(Taylor & Francis Inc, 2007)
Geological and geochemical characteristics of the Mid-Cretaceous olistostromal ophiolitic melange exposed in the southern part of the eastern Pontide magmatic arc indicates that it originally formed during the drifting ...
Three-directional extensional deformation and formation of the Liassic rift basins in the Eastern Pontides (NE Turkey)
(Slovak Acad Sciences Geological Inst, 2006)
The Eastern Pontide magmatic arc (NE Turkey) was rifted by the polyphase extensional tectonic regimes in the Early Jurassic. While alternated volcanics and siliciclastic sedimentary rocks accumulated during the episodic ...
Determination of Tectonic and Crustal Structure of the Eastern Pontide Orogenic Belt (NE Turkey) Using Gravity and Magnetic Data
(Springer Basel Ag, 2009)
The Eastern Pontide Orogenic Belt is one of the most complex geodynamic settings within the Alpine belt. Subduction polarity, which is responsible for the formation of the Eastern Pontide Magmatic Arc, is still under debate ...