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Cekic Dagi Formation

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Journal Article
Published: 01 October 2007
Journal of Foraminiferal Research (2007) 37 (4): 360–371.
... ). Other units are allochthonous and tectonically overlie each other and the autochthon above low angle thrust faults. Özgül (1997) named the Permian strata of the Aladag Unit the Cekic Dagi Formation. They are more than 1000 m thick and contain in their middle part the new genus Necdetina (Figs...
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Journal Article
Journal: GSA Bulletin
Published: 01 May 2009
GSA Bulletin (2009) 121 (5-6): 954–956.
... base of a 20-cm-thick grainstone that caps the bioclastic packstones of the Cekic Dagi Formation ( Unal et al., 2003 ). However, at this location, Payne et al. (2007) identify three potential dissolution surfaces developed within the upper 10 cm of the grainstone, although the illustration...
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Journal Article
Published: 01 April 2007
Journal of Micropalaeontology (2007) 26 (1): 73–85.
... Formation) and Permian (Cekic Dagi Formation) deposits of the Aladag Unit were carried out by Ozgul (1997 ). Foraminiferal faunas and biozones of the Yaricak Formation (Carboniferous) were also presented in great detail by Altiner & Ozgul (2001 ). The Taurides, one of the major units...
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Journal Article
Journal: PALAIOS
Published: 01 September 2015
PALAIOS (2015) 30 (9): 714–727.
... of these areas is similar to the TOH, with most of the occurrences of oolites from the P–Tr transition interval. There are 10 formations bearing oolites ( Table 2 ). The well-studied cases are the Taşkent section and the Çürük Dag section. The Çekiç Dagi and Yülük Tepe formations belong to the end-Permian...
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Series: Society of Exploration Geophysicists Distinguished Instructor Series
Published: 01 January 2006
DOI: 10.1190/1.9781560801979.ch1
EISBN: 9781560801979
... bk. Genellikle P dalgası hızı için kullanılır. α || : Simetri eksenine paralel doğrultudaki P dalgası hızı. Thomsen anisotropic parameters 'e bk. AAPG-A : Jeolojik ve petrol verilerini birinden diğerine değiştirmek için kullanılan format. Shaw and Walker (1989) 'a bk. A+B, A*B : AVO...
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