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Sivas Basin

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Series: Geological Society, London, Special Publications
Published: 14 April 2020
DOI: 10.1144/SP490-2019-92
EISBN: 9781786205155
...Abstract Abstract The Sivas Basin in central-eastern Anatolia is a north-verging salt-bearing fold-and-thrust belt including synorogenic salt tectonics. It formed between the northern leading edge of the Taurides platform and the Kırşehir block since Late Cretaceous time. We have constructed...
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Journal Article
Journal: Interpretation
Published: 15 June 2016
Interpretation (2016) 4 (3): SM17–SM31.
... of the diapiric structures and associated stratigraphy. In this paper, we focus on the Inceyol minibasin located in the Sivas Basin, Turkey. The high-quality but sparse information and the complex geometries observed at outcrop present a real challenge for 3D geologic model building. Our purpose is mainly...
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Journal Article
Published: 01 January 2014
Bulletin de la Société Géologique de France (2014) 185 (1): 33–42.
...Jean-Paul Callot; Charlotte Ribes; Charlie Kergaravat; Cédric Bonnel; Haluk Temiz; André Poisson; Bruno Vrielynck; Jean-François Salel; Jean-Claude Ringenbach Abstract The Sivas basin (Turkey) shows pronounced salt tectonics activity involving the Oligocene evaporites. Despite the complete exposure...
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Journal Article
Published: 01 June 2006
Clays and Clay Minerals (2006) 54 (3): 333–350.
... the Yagmurluseki area in the Sivas Basin: (a) layered and lens-shaped talc within thin claystones surrounded by the coarse-grained siliciclastic rocks; (b) nodular talc within the gravelly marl. * E-mail address of corresponding author: yalcin@cumhuriyet.edu.tr 18 04 2005 15 12 2005 ©...
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Modeling of the isostatic response of the <b>Sivas</b> <b>Basin</b> to incision. (A) Dept...
Published: 02 April 2021
Figure 7. Modeling of the isostatic response of the Sivas Basin to incision. (A) Depth of incision of the Sivas basin floor, and corresponding isostatic rebound (contour line spacing = 25 m) for a lithospheric elastic thickness of 10 km (map location on Fig. 2A ). White lines—proven active
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Modeling of the isostatic response of the <b>Sivas</b> <b>Basin</b> to incision. (A) Dept...
Published: 02 April 2021
Figure 7. Modeling of the isostatic response of the Sivas Basin to incision. (A) Depth of incision of the Sivas basin floor, and corresponding isostatic rebound (contour line spacing = 25 m) for a lithospheric elastic thickness of 10 km (map location on Fig. 2A ). White lines—proven active
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The case of the central <b>Sivas</b> <b>Basin</b>, a minibasin province. (A) Regional com...
Published: 01 September 2016
Figure 14. The case of the central Sivas Basin, a minibasin province. (A) Regional composite lithostratigraphic column showing the average thickness of the various stratigraphic units in the central Sivas Basin. (B) Geological map of the central Sivas Basin, showing the locations of salt outcrops
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Location of the <b>Sivas</b> <b>Basin</b> and the Inceyol minibasin. (a) Tectonic map of ...
Published: 15 June 2016
Figure 2. Location of the Sivas Basin and the Inceyol minibasin. (a) Tectonic map of Turkey, with the main continental blocks, major suture zones and Oligo-Miocene Sivas Basin deposits (adapted from Ribes et al., 2015 ). (b) Location of the Inceyol minibasin in the geologic setting of the Sivas
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A) Geographic setting of the <b>Sivas</b> <b>basin</b> (NAFZ: North Anatolian Fault zone;...
Published: 01 January 2014
Fig. 1 A) Geographic setting of the Sivas basin (NAFZ: North Anatolian Fault zone; SAFZ: South Anatolian Fault zone). B) Geologic map of the Sivas basin adapted from Poisson et al . [1996] and Ciner et al . [2002].
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Geological map of the central <b>Sivas</b> <b>basin</b> (see  figure 1  for location) sho...
Published: 01 January 2014
Fig. 2 Geological map of the central Sivas basin (see figure 1 for location) showing the main gypsum outcrops, the major minibasins and bed dips within. Note the polygonal geometry of the gypsum walls, symptomatic of gravity driven sedimentary spreading ontop a thick ductile level. The southern
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Synthetic lithostratigraphic log of the major minibasin of the <b>Sivas</b> <b>basin</b> ...
Published: 01 January 2014
Fig. 3 Synthetic lithostratigraphic log of the major minibasin of the Sivas basin (namely Emirhan and Karayün), with the main unit and formation name (see also fig. 6 ).
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A: Distribution of gypsum outcrops at the <b>Sivas</b> <b>basin</b> scale. B: Enlargement...
Published: 01 January 2014
Fig. 4 A: Distribution of gypsum outcrops at the Sivas basin scale. B: Enlargement of the gypsum distribution in the core area of the basin, which shows the most prominent minibasins and the general polygonal pattern of evaporite distribution. C: Distribution of the shallow salt bodies
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Geological map of the southern part of the <b>Sivas</b> <b>Basin</b> (prepared after  Yil...
Published: 01 June 2006
Figure 2. Geological map of the southern part of the Sivas Basin (prepared after Yilmaz et al. , 1989 ; Poisson et al. , 1996 ; Kavak, 1998 ; Gökten, 1993 ).
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Talc occurrences from the Yagmurluseki area in the <b>Sivas</b> <b>Basin</b>: (a) layered...
Published: 01 June 2006
Figure 4. Talc occurrences from the Yagmurluseki area in the Sivas Basin: (a) layered and lens-shaped talc within thin claystones surrounded by the coarse-grained siliciclastic rocks; (b) nodular talc within the gravelly marl.
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a) Location of the Tertiary <b>Sivas</b> <b>Basin</b> in Turkey. b) Location map of the s...
Published: 01 June 2002
F ig . 1. a) Location of the Tertiary Sivas Basin in Turkey. b) Location map of the study area in the Sivas Basin. c) Simplified geological map of the study area and location of celestine – barite – (Ba,Sr)SO 4 beds.
Journal Article
Published: 01 June 2002
The Canadian Mineralogist (2002) 40 (3): 895–908.
...F ig . 1. a) Location of the Tertiary Sivas Basin in Turkey. b) Location map of the study area in the Sivas Basin. c) Simplified geological map of the study area and location of celestine – barite – (Ba,Sr)SO 4 beds. ...
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Drainage of some lacustrine carbonates located in the areas of Lake Seyfe (...
Published: 02 April 2021
Figure 14. Drainage of some lacustrine carbonates located in the areas of Lake Seyfe (A), eastern Sivas Basin (B), central Sivas Basin (C), and Tuz Lake basin (D). Locations are shown on Figure 2B . Cap carbonate scarp retreat (gray arrows) occurs by landsliding (C) and headward stream erosion
Series: GSA Special Papers
Published: 01 January 2006
DOI: 10.1130/2006.2409(21)
... of the late Cenozoic deformation in eastern Anatolia, the main ar gument is that the region was subjected largely to extension and strike-slip tectonics Compression was limited to the narrow eastern Taurus belt and to a north-south strip comprising the Afsin and Gürün arcs and the Sivas basin. This is shown...
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Chronostratigraphic diagram comparing geohistory of the Tuzgölü, Şarkış...
Published: 01 December 2002
Fig. 16.  Chronostratigraphic diagram comparing geohistory of the Tuzgölü, Şarkışla and Sivas basins. Tuzgölü Basin stratigraphy from Çemen et al . (1999) , Şarkışla Basin stratigraphy from Gökten (1986) and Sivas basin from Dirik et al . (1999) .
Series: Geological Society, London, Special Publications
Published: 01 January 2007
DOI: 10.1144/SP291.13
EISBN: 9781862395398
... fissures and at a rate an order higher than for bedded travertine on the surface. Earthquakes of magnitude M≤4 occur too frequently in the Sivas Basin to have any apparent influence on travertine deposition but earthquakes with M in the range 4.5–5.5 occur with a frequency compatible with the travertine...
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