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Ulukisla Basin

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Journal Article

The role of the Early Tertiary Ulukisla Basin, southern Turkey, in suturing of the Mesozoic Tethys ocean Available to Purchase

Matthew Clark, Alastair Robertson
Published: 01 December 2002
Journal of the Geological Society (2002) 159 (6): 673–690.
DOI: https://doi.org/10.1144/0016-764902-015
...Matthew Clark; Alastair Robertson Abstract The Maastrichtian–Late Eocene Ulukisla Basin is representative of the tectonic and sedimentary evolution of prominent Early Tertiary basins in central Anatolia, including the Tuzgölü and Şarkışla basins. The Ulukisla Basin overlies an ophiolitic...
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View PDF for article title, The role of the Early Tertiary <span class="search-highlight">Ulukisla</span> <span class="search-highlight">Basin</span>, southern Turkey, in suturing of the Mesozoic Tethys ocean
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 Revised stratigraphy of the Ulukisla Basin. (See text for discussion.) Initial palaeontological dating was carried out mainly by Oktay (1973, 1982) and Demirtașlı et al. (1984), with recent revision by N. I2nan and K. Taslı of Mersin University. (See Fig. 3 for key.) Previous stratigraphies have been given by Oktay (1973, 1982), Demirtașlı et al. (1984) and (Çevikbaș &amp; Özuntalı 1991). Subdivisions of the Aktaștepe Formation: GD, Güneydagı Member; KK, Kalkankaya Member; ÖM, Ömerli Member; subdivisions of the Hasangazi Formation: GM, Gümüș Member; BM, Basmakçı Member.

Revised stratigraphy of the Ulukisla Basin. (See text for discussion.) Init... Available to Purchase

Published: 01 December 2002
Fig. 4.  Revised stratigraphy of the Ulukisla Basin. (See text for discussion.) Initial palaeontological dating was carried out mainly by Oktay (1973, 1982) and Demirtașlı et al . (1984) , with recent revision by N. I2nan and K. Taslı of Mersin University. (See Fig. 3 for key.) Previous
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 Simplified geological map of the Ulukisla Basin based on this study andDemirtașlı et al. (1984). (See text for locality descriptions and Fig. 14 for cross-sections.)

Simplified geological map of the Ulukisla Basin based on this study and Dem... Available to Purchase

Published: 01 December 2002
Fig. 3.  Simplified geological map of the Ulukisla Basin based on this study and Demirtașlı et al . (1984) . (See text for locality descriptions and Fig. 14 for cross-sections.)
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 Subsidence curve plotted from composite log of the Ulukisla Basin succession, data from the Gümüș area. The lack of any major unconformities in the Maastrichtian to Oligocene succession allows construction of the curve. Both the water-depth estimates and the dating of the rocks are possible sources of error. Total decompaction subsidence was calculated using the approach of Steckler &amp; Watts (1978). Each layer of rock was removed to reconstruct the total subsidence history of the basin and remaining layers were decompacted using standard porosity–depth relationships determined by Sclater &amp; Christie (1980). The ‘zero’ level for depth equates to local sea level at the beginning of the basin history.

Subsidence curve plotted from composite log of the Ulukisla Basin successio... Available to Purchase

Published: 01 December 2002
Fig. 12.  Subsidence curve plotted from composite log of the Ulukisla Basin succession, data from the Gümüș area. The lack of any major unconformities in the Maastrichtian to Oligocene succession allows construction of the curve. Both the water-depth estimates and the dating of the rocks
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 Existing models for the Ulukisla Basin and the Inner Tauride Ocean: (a) fore-arc basin associated with Tuzgölü Basin (Görür et al. 1984); (b) island-arc model (Oktay 1982); (c) Tauride promontory without Inner Tauride Ocean (Göncüoglu 1986;Göncüoglu et al. 1992).

Existing models for the Ulukisla Basin and the Inner Tauride Ocean: ( a ) f... Available to Purchase

Published: 01 December 2002
Fig. 15.  Existing models for the Ulukisla Basin and the Inner Tauride Ocean: ( a ) fore-arc basin associated with Tuzgölü Basin ( Görür et al . 1984 ); ( b ) island-arc model ( Oktay 1982 ); ( c ) Tauride promontory without Inner Tauride Ocean ( Göncüoglu 1986 ; Göncüoglu et al . 1992) .
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 Structural cross-sections of the Ulukisla Basin (see Fig. 4 for location of cross-sections and key to symbols).

Structural cross-sections of the Ulukisla Basin (see Fig. 4 for location ... Available to Purchase

Published: 01 December 2002
Fig. 13.  Structural cross-sections of the Ulukisla Basin (see Fig. 4 for location of cross-sections and key to symbols).
Journal Article

Cenozoic tectonic evolution of the Ecemiş fault zone and adjacent basins, central Anatolia, Turkey, during the transition from Arabia-Eurasia collision to escape tectonics Open Access

Paul J. Umhoefer, Stuart N. Thomson, Côme Lefebvre, Michael A. Cosca, Christian Teyssier, Donna L. Whitney
Journal: Geosphere
Published: 27 October 2020
Geosphere (2020) 16 (6): 1358–1384.
DOI: https://doi.org/10.1130/GES02255.1
... basin, and metamorphic dome (Niğde Massif) record two fundamentally different stages in the Cenozoic tectonic evolution of this part of central Anatolia. The Paleogene sedimentary and volcanic strata of the NE Ulukışla basin (Ecemiş corridor) were deposited in marginal marine to marine environments...
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View PDF for article title, Cenozoic tectonic evolution of the Ecemiş fault zone and adjacent <span class="search-highlight">basins</span>, central Anatolia, Turkey, during the transition from Arabia-Eurasia collision to escape tectonics
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CLAST DATA FROM ALLUVIAL DEPOSITS IN THE ECEMIŞ AND ULUKIȘLA BASINS Open Access

Published: 09 August 2017
TABLE 4. CLAST DATA FROM ALLUVIAL DEPOSITS IN THE ECEMIŞ AND ULUKIȘLA BASINS
Journal Article

Structural Evolution of the Tuzgölü Basin in Central Anatolia, Turkey Available to Purchase

İbrahim Çemen, M. Cemal Göncüoglu, Kadir Dirik
Published: 01 November 1999
The Journal of Geology (1999) 107 (6): 693–706.
DOI: https://doi.org/10.1086/314379
... the Central Anatolian thrust belt to the north and the late Eocene south-dipping thrust faults of the Ulukişla basin to the south. This reactivation is suggested by structurally repeated and missing Paleocene-Eocene deposits in some of the basin's wildcat wells. The late Eocene regression in the Tuzgölü basin...
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View PDF for article title, Structural Evolution of the Tuzgölü <span class="search-highlight">Basin</span> in Central Anatolia, Turkey
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 Equal-area stereographic plots of poles to bedding, poles to profile planes and poles to fault planes for the Ulukisla Basin: (a) poles to bedding for the Ulukisla Basin; (b) poles to bedding from area around Maden and Hasangazi; (c) poles to bedding from Çakillar area; (d) poles to bedding from Basmakçı to locality 16; (e) fold at Bozbeltepe; (f) fold at Kalkankaya; (g) fold from east of locality 19 (Fig. 3); (h) poles to profile planes from above stereographic projections; (i) poles to fold axial planes; (j) poles to planes of reverse faults.

Equal-area stereographic plots of poles to bedding, poles to profile planes... Available to Purchase

Published: 01 December 2002
Fig. 14.  Equal-area stereographic plots of poles to bedding, poles to profile planes and poles to fault planes for the Ulukisla Basin: ( a ) poles to bedding for the Ulukisla Basin; ( b ) poles to bedding from area around Maden and Hasangazi; ( c ) poles to bedding from Çakillar area; ( d
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 Palaeocurrent data (azimuthal) from turbiditic sandstones of the Halkapınar Formation, measured from cross-bedding and flute casts: (a) Gümüș area (Fig. 3, localities 6 and 7); (b) Çakillar area (Fig. 3, localities 5–8); (c) Ulukisla Basin as a whole.

Palaeocurrent data (azimuthal) from turbiditic sandstones of the Halkapınar... Available to Purchase

Published: 01 December 2002
Fig. 7.  Palaeocurrent data (azimuthal) from turbiditic sandstones of the Halkapınar Formation, measured from cross-bedding and flute casts: ( a ) Gümüș area ( Fig. 3 , localities 6 and 7); ( b ) Çakillar area ( Fig. 3 , localities 5–8); ( c ) Ulukisla Basin as a whole.
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 Major sedimentary basins of central Anatolia, with Bolkar Carbonate Platform (BP) and Nigde–Kırşehir Massif (NKM) also shown. UB, Ulukisla Basin; TB, Tuzgölü Basin; HB, Haymana Basin; KKB, Kırıkkale Basin; CB, Çankiri Basin; YSB, Yozgat–Sorgun Basin; KB, Kizilirmak Basin; YB, Yildizli Basin; RB, Refahiye Basin; SB, Sivas Basin; SKB, Şarkışla Basin; EFZ, Ecemiș Fault Zone. (Adapted from Görür et al. 1998.)

Major sedimentary basins of central Anatolia, with Bolkar Carbonate Platfor... Available to Purchase

Published: 01 December 2002
Fig. 2.  Major sedimentary basins of central Anatolia, with Bolkar Carbonate Platform (BP) and Nigde–Kırşehir Massif (NKM) also shown. UB, Ulukisla Basin; TB, Tuzgölü Basin; HB, Haymana Basin; KKB, Kırıkkale Basin; CB, Çankiri Basin; YSB, Yozgat–Sorgun Basin; KB, Kizilirmak Basin; YB
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Index map showing major basins and tectonic elements of Central Anatolia. A=Ankara; CACC=Central Anatolian Crystalline Complex; CB=Cankiri basin; EAFZ=East Anatolian fault zone; EFZ=Ecemis fault zone; DSFZ=Dead Sea fault zone; GV=Galatian Volcanics; BB=Haymana basin; IAS = İzmir-Ankara suture zone; IPS=Intrapontide suture zone; KBBU = Kütahya-Bolkardaği belt units; UB=Ulukisla basin; SB=Sivas basin; TGB = Tuzgölü basin.

Index map showing major basins and tectonic elements of Central Anatolia. ... Available to Purchase

Published: 01 November 1999
F Z = Dead Sea fault zone; G V = Galatian Volcanics; B B = Haymana basin; IAS = İzmir-Ankara suture zone; I P S = Intrapontide suture zone; KBBU = Kütahya-Bolkardaği belt units; U B = Ulukisla basin; S B = Sivas basin; TGB
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Map of some major geologic features of Central Anatolia, including metamorphic and granitic rocks of the Central Anatolian Crystalline Complex (CACC); fragments of the Central Anatolian Ophiolite (Çiçekdağ, Kaman, Kurancalı, Kuştepe, Ortaköy, and Sarıkaraman), Tauride Ophiolites (Alihoca and Pozantı-Karsantı), and the Niğde Mafic Complex (NMC); the Tauride Mountains (carbonate platform units); Cappadocian volcanic province (including two stratovolcanoes: Erciyes and Hasan Dağı); Neotethyan suture zones (İzmir-Ankara-Erzıncan and Inner Tauride); fault zones (Central Anatolian fault zone and its southern segment, the Ecemiş fault; Tuz Gölü fault); and the Ulukışla Basin.

Map of some major geologic features of Central Anatolia, including metamorp... Open Access

Published: 09 August 2017
zone and its southern segment, the Ecemiş fault; Tuz Gölü fault); and the Ulukışla Basin.
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Geologic map and tectonostratigraphic columns of the Niğde-Çamardı-Ecemiş fault zone study area with the Niğde Massif to the west, Tauride Mountains to the east, and the northeastern Ulukışla basin (Ecemiş corridor) between them. The Ecemiş fault zone is the left lateral fault zone on the western edge of the Tauride Mountains. Dotted white rectangles indicate location of detailed maps presented in Figures 4–8. Dotted thick black line indicates the trace of the cross section of Figure 9. The red, green, and blue ages adjacent to the yellow sample numbers are the apatite fission-track ages as interpreted on Figure 13 and in the text as cooling ages, partially reset ages, and detrital ages, respectively. The 59 Ma age in yellow next to the yellow star is the 40Ar/39Ar age. White abbreviations are the villages of Ba—Bademdere, Bu—Burç, Ç—Çamardı, D—Demirkazık, E—Elekgölü, P—Pinarbaşı. The large city of Niğde is on the left.

Geologic map and tectonostratigraphic columns of the Niğde-Çamardı-Ecemiş f... Open Access

Published: 27 October 2020
Figure 3. Geologic map and tectonostratigraphic columns of the Niğde-Çamardı-Ecemiş fault zone study area with the Niğde Massif to the west, Tauride Mountains to the east, and the northeastern Ulukışla basin (Ecemiş corridor) between them. The Ecemiş fault zone is the left lateral fault zone
Journal Article

Ophiolite gabbro from source to sink: A record of tectonic and surface processes in Central Anatolia Open Access

Molly Radwany, Donna L. Whitney, Gilles Brocard, Paul J. Umhoefer, Christian Teyssier
Journal: Geosphere
Published: 09 August 2017
Geosphere (2017) 13 (5): 1329–1358.
DOI: https://doi.org/10.1130/GES01465.1
...TABLE 4. CLAST DATA FROM ALLUVIAL DEPOSITS IN THE ECEMIŞ AND ULUKIȘLA BASINS ...
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View PDF for article title, Ophiolite gabbro from source to sink: A record of tectonic and surface processes in Central Anatolia
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Journal Article

First occurrence of the genus Zonocypris (Ostracoda) in the Pleistocene of Western Europe (Portugal) Available to Purchase

M. C. CABRAL, J.-P. COLIN, P. CARBONEL
Published: 01 November 2004
Journal of Micropalaeontology (2004) 23 (2): 105–106.
DOI: https://doi.org/10.1144/jm.23.2.105
... in Kurtulmustepe Formation of Ulukisla Basin (Turkey) . Revista Espaňola de Micropaleontologia , 24 : 63 – 69 . Schäfer , H.W. 1952 . Über Süßwasser-Ostracoden aus der Türkei . Veröffentlichungen des Forschungsinstituts für Hydrobilogie der Natur-wissenschaftlichen Fakultät der Universität Instanbul...
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View PDF for article title, First occurrence of the genus Zonocypris (Ostracoda) in the Pleistocene of Western Europe (Portugal)
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Mineralogy, geochemistry, and Sr–Nd isotopes of the Cretaceous leucogranite from Karamadazı (Kayseri), central Turkey: implications for their sources and geological setting Available to Purchase

Kerim Kocak
Published: 30 September 2008
Canadian Journal of Earth Sciences (2008) 45 (8): 949–968.
DOI: https://doi.org/10.1139/E08-040
.... Boztuğ D. Frei R. Temel A. Kurt M.A. 2006 Geochemical and Pb–Sr–Nd isotopic composition of the ultrapotassic volcanic rocks from the extension-related Çamardı-Ulukışla basin, Niğde Province, Central Anatolia, Turkey. Journal of Asian Earth Sciences 27 613 627 10.1016/j.jseaes...
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View PDF for article title, Mineralogy, geochemistry, and Sr–Nd isotopes of the Cretaceous leucogranite from Karamadazı (Kayseri), central Turkey: implications for their sources and geological setting
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Journal Article

Evolution of mafic lavas in Central Anatolia: Mantle source domains Open Access

Tanya Furman, Barry B. Hanan, Megan Pickard Sjoblom, Biltan Kürkcüoğlu, Kaan Sayit, Erdal Şen, Pinar Alıcı Şen, Tekin Yürür
Journal: Geosphere
Published: 04 November 2021
Geosphere (2021) 17 (6): 1631–1646.
DOI: https://doi.org/10.1130/GES02329.1
.... 1022 – 1041 , https://doi.org/10.2747/0020-6814.46.11.1022 . Alpaslan , M. , Boztuğ , D. , Frei , R. , Temel , A. , and Kurt , M.A. , 2006 , Geochemical and Pb-Sr-Nd isotopic composition of the ultrapotassic volcanic rocks from the extension-related Çamardı-Ulukışla basin...
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(A) Geologic map of the Niğde area, showing major features including the Niğde Massif; the Niğde Mafic Complex and other outcrops of mafic and ultramafic rocks; and the Ulukışla and Ecemiş basins. Sample locations are shown for the three main sample populations: outcropping rocks of the Niğde Mafic Complex and associated rocks, clasts in Çukurbağ conglomerate, and cobbles on alluvial terraces. (B) Representative cross sections through the Niğde Mafic Complex (NMC): NW-SE (section A–A′) and NE-SW (section B–B′). Locations of detailed geologic maps (Figs. 6A–6D) and clast count map (Fig. 9) are indicated.

(A) Geologic map of the Niğde area, showing major features including the Ni... Open Access

Published: 09 August 2017
Figure 3. (A) Geologic map of the Niğde area, showing major features including the Niğde Massif; the Niğde Mafic Complex and other outcrops of mafic and ultramafic rocks; and the Ulukışla and Ecemiş basins. Sample locations are shown for the three main sample populations: outcropping rocks