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Diachronous initiation of Arabia–Eurasia collision from eastern Anatolia to the southeastern Zagros Mountains since middle Eocene time
The persistent debate over the timing of initial Arabia–Eurasia collision has eluded
consensus for decades, with most estimates ranging widely from~ 50 to 10 Ma along both …
consensus for decades, with most estimates ranging widely from~ 50 to 10 Ma along both …
Palaeogene stratigraphy and chronology of the western Sivas Basin, central Anatolia (Turkey): Tectono‐sedimentary evolution of a well‐preserved basin along the …
Abstract The Sivas Basin overlaps the northern Neotethys suture zone in central Anatolia
(Turkey) and contains a ca. 12‐km thick succession of Cenozoic strata that provides an …
(Turkey) and contains a ca. 12‐km thick succession of Cenozoic strata that provides an …
[HTML][HTML] Shortening and extrusion in the East Anatolian Plateau: How was Neogene Arabia-Eurasia convergence tectonically accommodated?
Deformation in orogenic belts is typically widely distributed but may be localized to form
discrete, fast-moving fault zones enclosing semi-rigid microplates. An example is the …
discrete, fast-moving fault zones enclosing semi-rigid microplates. An example is the …
Tectonic development of the Ankara-Erzincan suture and the eastern Pontide mountains, northeast Anatolia, Turkey
The Eastern Pontides are the northmost component of the Anatolian orogen. Its geological
development closely associated with the evolution of the Ankara-Erzincan Suture. It exhibits …
development closely associated with the evolution of the Ankara-Erzincan Suture. It exhibits …
Tectonic development of the Ankara-Erzincan suture and the Eastern Pontide mountains, Northeast Anatolia, Turkey
ABSTRACT The Eastern Pontides are the northeasternmost component of the Anatolian
orogen. Its geological development is closely associated with the evolution of the Ankara …
orogen. Its geological development is closely associated with the evolution of the Ankara …