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Regional significance of neotectonic counterclockwise rotation in central turkey
(1996)
Counterclockwise rotation is a characteristic feature of the results of most paleomagnetic studies of the Pontides and Anatolides of central Turkey, applicable to regions both north and south of the North Anatolian fault ...
Tectonostratigraphy and thrust tectonics of the central and eastern parts of the sivas tertiary basin, turkey
(1996)
The Sivas Tertiary Basin is one of the central Anatolian basins that formed over the collision zone between the Pontides and the Anatolide-Tauride belts. The basin, which is floored by southerly obducted Neotethyan ophiolite ...
Tectonic setting and evolution of the sivas basin, central anatolia, turkey
(1996)
The Sivas Basin is one of several Central Anatolian basins. It developed mainly after the closure of the northern branch of Neotethys. Its location between the Kirsehir Massif and the Taurides implies that it should not ...
Tectonics of the sivas basin: The neogene record of the anatolian accretion along the inner tauric suture
(1996)
The Sivas Basin extends over a major crustal structure underlying the contact zone between the Tauride and Pontide belts. The Kirsehir block, a continental crustal element lying between the main belts, introduces a subordinate ...