Yazar "Canbolat, M. Yasin" seçeneğine göre listele

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    Shallow Marine Benthic Foraminifera Assemblage of the Early Eocene Succession in the Northern Arac (Kastamonu) and Paleoecological Interpretation
    (TMMOB JEOLOJI MUHENDISLERI ODASI, 2016) Ozgen Erdem, Nazire; Canbolat, M. Yasin; Sinanoglu, Derya
    Soganli Formation of Early Eocene age in the northeastern of Arac (Kastamonu) has been investigated in order to determine their paleontology and palaeoecology. The sequence consists of gray, yellowish, clayey limestone, rich in larger benthic foraminifers. The lower parts of clayey limestone are dominated by porcellaneous foraminifera such as Alveolina and Orbitolites and by dascylad algae. The top of the section is characterized by hyaline calcareous foraminifers such as Assilina and Nummulites. Idalina sinjarica Grimsdale, Glomalveolina lepidula Schwager, A. cemali Sirel & Acar, A. rotundata kazancii Sirel & Acar, A. erki Acar, A. ankarensis Sirel, A. pieroi Sirel & Acar, Lockhartia conditi (Nuttall), L. tipperi (Davies), Orbitolites complanatus Lamarck, Cyclopertorbitolites tokerae Ozgen-Erdem, Assilina spinosa Davies & Pinfold, Nummulites sp., Cribrobulimina sp., Kathina sp., Neorotalia sp., Triloculina sp. have been decribed along the section. The distribution of the larger benthic foraminifera indicates Early Eocene age. According to these assemblages, we interpret that deposition of the unit started in a restricted shallower environment and continued in a shallow high energy environment.
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    The Upper Mesozoic Stratigraphy of Turhal, Pazar, Zile (Tokat) Region
    (Tmmob Jeoloji Muhendisleri Odasi, 2014) Yolcubal, Hulya Gureli; Akyazi, Mehmet; Sezen, T. Fikret; Toprak, Ozlem; Canbolat, M. Yasin; Kocak, Filiz; Ozkan, Aysegul
    The presences of base-cover separation are established as all Pontid Tectonic Belt when stratigraphic units are investigated in the studied area that is located at the northwest of Tokat city. Upper Mesozoic cover units are one of cover units located uncormably on base units and are interesting in terms of fossil content and diversity. In this study, these units are dated as detail and stratigraphy of region is constructed according to these ages. In addition, data of the geologic and stratigraphic positions of study area are observed.