Tecer Formation

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Journal Article
Published: 01 January 2003
Micropaleontology (2003) 49 (2): 201–204.
... in Upper Danian levels of Gölköy formation (Ordu) ( Meriç and Ýnan 1998 ). Ýnan and Ýnan (1987 and 1990) found it with Laffitteina erki, Laffitteina bibensis, and Scandonea aff. S. samnitica De Castro in the Upper Danian level of the Tecer Formation in Tecer Mountain (Sivas...
Journal Article
Published: 01 June 2006
Clays and Clay Minerals (2006) 54 (3): 333–350.
... Jurassic–early Cretaceous age ( Inan et al. , 1993 ), the Divrigi ophiolitic complex of late Cretaceous age ( Tunç et al. , 1991 ) and the Tecer formation of late Cretaceous-early Paleocene age ( Inan and Inan, 1990 ) form the basement of the Sivas Basin. The ophiolitic series consists mainly...
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Series: Geological Society, London, Special Publications
Published: 14 April 2020
DOI: 10.1144/SP490-2019-92
EISBN: 9781786205155
... of Bozbel Formation. ( b ) Panoramic view of the Karacalar Anticline used to control the formations in subsurface. ( c ) Ophiolite thrust capped by Maastrichtian limestones (Tecer Formation) over Eocene turbidites (Bozbel Formation) belonging to the Southern edge. ( d ) Thrusted evaporites between a primary...
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Journal Article
Published: 12 August 2022
Bulletin de la Société Géologique de France (2022) 193 (1): 12.
... et al. , 2000 ). The ophiolite was obducted between the late Santonian and pre-late Campanian. It is covered by sedimentary successions consisting of Maastrichtian to Thanetian shallow-water platform carbonates (Tecer Formation: İnan and İnan, 1990 ; Legeay et al. , 2019 ), changing northward...
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Journal Article
Published: 01 July 2003
Journal of Foraminiferal Research (2003) 33 (3): 273–274.
.../English abstract).—“Foraminifera are described from the La Barca Formation, a 220 m thick upwards fining, organic-rich sequence on Peninsula Mitre, Tierra del Fuego. . . Its lower member bears a peculiar assemblage of calcareous benthic foraminifera, here called the Bulimina karpatica Assemblage...
Journal Article
Published: 29 September 2017
Quarterly Journal of Engineering Geology and Hydrogeology (2017) 50 (4): 402–411.
... of this lithotype, Oira stone, was conducted. This stone was employed during the 19th century restoration of the façade, and the on-site evaluation of the stone blocks after more than a century of exposure showed a distinctive chromatic alteration. The formation of a fragile superficial layer with scaling...
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Journal Article
Published: 01 January 2006
Micropaleontology (2006) 52 (3): 281–286.
... limestones; 7- Eocene Foraminiferal limestones; 8 - Eocene Breccias with fragments of Foraminiferal limestones; 9 - Middle Eocene Flysch; 10 - Oligocene clastic deposits. A 35m thick brecciated formation, named the Tilovica breccia, has been studied in detail. It uncomformably overlies (transgressive...
Journal Article
Published: 01 June 2002
The Canadian Mineralogist (2002) 40 (3): 895–908.
... into four categories. These are void-filling, zebra, nodular, and massive celestine deposits. The first type is found in dark brown turbiditic limestones in the upper parts of the Middle to Late Eocene Bozbel Formation. The second type, the zebra deposits, has bands a few cm to a few meters in thickness...
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Series: Geological Society, London, Special Publications
Published: 01 January 2013
DOI: 10.1144/SP372.16
EISBN: 9781862396357
... are unconformably overlain by shallow-marine mixed carbonate-clastic facies (i.e. Tecer Formation of Atabey & Aktimur 1997 ; İnan & İnan 1988 ). A basal conglomerate (<10 m thick) is well exposed along the northern margin of Tecer Dağ (e.g. near Esentepe). This is dominated by subrounded to sub-angular...
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Journal Article
Journal: Geosphere
Published: 02 April 2021
Geosphere (2021) 17 (3): 739–765.
... of sedimentation across the plateau would therefore mark the opening of these closed catchments, their integration, and the formation of the present-day drainage. By combining newly dated volcanic markers with previously dated sedimentary sequences, we show that this drainage integration occurred remarkably...
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Series: GSA Special Papers
Published: 01 January 2006
DOI: 10.1130/2006.2409(21)
... plate ( Biju-Duval et al., 1977 ; Livermore and Smith, 1984 ; Yazgan and Chessex, 1991 ). Arabia and part of Africa collided with Eurasia, resulting in the closure of the southern branch of the Neo-Tethys and the formation of the eastern Taurus belt. An oceanic or thin continental lithosphere...