Browsing by Author "Poisson A."
Now showing items 1-6 of 6
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New stratigraphic data concerning the marine Oligo-Miocene formations of the Sivas Basin (Turkey) [Nouvelles données stratigraphiques concernant les formations oligo-miocènes marines du bassin de Sivas (Turquie)]
Poisson A.; Wernli R.; Lozouet P.; Poignant A.; Temiz H. (Elsevier Masson SAS, 1997)The stratigraphy of the marine Oligo-Miocene formations of the Sivas basin has been revised on the basis ofplanktic and benthic fauna and microfauna. In the Sivas area, three of the main structural units present three ... -
Recent temporal change in the stress state and modern stress field along the North Anatolian Fault zone (Turkey)
Bellier O.; Över S.; Poisson A.; Andrieux J. (Oxford University Press, 1997)The North Anatolian Fault (NAF) is a dextral strike-slip fault which runs about 1400 km from east to west, from the Karliova triple junction to the Aegean domain. It was active during the Plio-Quaternary as a consequence ... -
Tectonic setting and evolution of the sivas basin, central anatolia, turkey
Poisson A.; Guezou J.C.; Ozturk A.; Inan S.; Temiz H.; Gürsöy H.; Kavak K.S.; Özden S. (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
Guezou J.-C.; Temiz H.; Poisson A.; Gürsoy H. (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 ... -
Tectonostratigraphic relationships between the North Anatolian Thrust Zone (NATZ), and the Kirsehir Massif to the north of Sivas (Turkey)
Özden S.; Poisson A.; Öztürk A.; Bellier J.P.; Blondeau A.; Wernli R. (Elsevier Masson SAS, 1998)In Central Anatolia, to the north of Sivas, the remains of the Northern Neotethyan domain crops out in a system of south verging thrust slices intercalated between the Eurasiatic margin (Tokat Massif), and the Taurus. In ... -
Tectonostratigraphy of the southern sivas tertiary basin (central turkey) and comparison with landsat mss imagery
Kavak K.S.; Poisson A.; Guezou J.C. (1997)The Sivas Basin is one of the most important sedimentary basins, in terms of tectonics and hydrocarbon potential, in the Central Anatolian region of Turkey. Its development is related mainly to the closure of the northern ...