Zobrazeno 1 - 10
of 33
pro vyhledávání: '"Cengiz Okuyucu"'
Autor:
AYŞE ATAKUL-ÖZDEMIR, ASUMAN GÜNAL-TÜRKMENOĞLU, M. CEMAL GÖNCÜOĞLU, ÖMER BOZKAYA, CENGIZ OKUYUCU
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 130, Iss 3 (2024)
New evidence for a biostratigraphic assessment of the limestone succession comprising K‐bentonite levels exposed in the Yılanlı Formation of the Istanbul-Zonguldak Terrane are provided from conodonts at the Gavurpınarı quarry in Bartın area (N
Externí odkaz:
https://doaj.org/article/9f4e6c19bb8d43cf89a25f54d719cc23
Publikováno v:
Estonian Journal of Earth Sciences, Vol 63, Iss 4, Pp 227-232 (2014)
The Karadere area to the east of Safranbolu in NW Anatolia is one of the very few localities in Turkey where the contact between the Cadomian basement and the Lower Palaeozoic transgressive succession is well exposed. The Ordovician graptolite Rhabdi
Externí odkaz:
https://doaj.org/article/352f8a80e0b14b32aeda51ee168d7097
Autor:
CENGIZ OKUYUCU
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 105, Iss 3 (1999)
The Hadim Nappe Carboniferous-Permian boundary and its fusulinacean-rich strata from the Çatalkatran Tepe stratigraphic section were studied. The appearance of Sphaeroschwagerina sp. determines the Carboniferous-Permian boundary in this section. The
Externí odkaz:
https://doaj.org/article/5974757e53544bdf9bd345321ecce213
Autor:
Cengiz Okuyucu, Melikan Akbas
Publikováno v:
PalZ. 96:517-541
Autor:
Cengiz Okuyucu, Melikan Akbaş
Publikováno v:
Journal of Paleontology. 95:476-496
The Hadim Nappe, which is one of the allochthonous tectonic units in the Tauride Belt, in southern Turkey, includes a continuous stratigraphic succession from the Middle(?)–Late Devonian to Late Cretaceous. A relatively complete succession of the u
Autor:
Cengiz Okuyucu
Publikováno v:
Micropaleontology. 67:557-564
The Karakaya Complex in northern Turkey is classically subdivided into two units (Upper and Lower Karakaya Complex) and located in the Sakarya Composite Terrane. The Upper Karakaya Complex includes different blocks and tectonic slices within a Triass
Publikováno v:
Facies. 68
Publikováno v:
Geobios. 59:61-77
The Mersin Melange (MM) as a part of the Mersin Ophiolitic Complex in southern Turkey is a sedimentary complex including blocks and tectonic slices within a Late Cretaceous matrix. Two blocks (Keven and Cingeypinari) within the MM originated from the
Five thin (5-15 cm) and yellowish green tephra (K-bentonite) layers are exposed along two sections in the south of Aksehir (Konya, southern Turkey) within the Early Carboniferous (Mississippian) red dolomite-dolomitic limestone succession of the Sult
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7a35920eaa42e86c82d17355d0c70f0f
https://hdl.handle.net/11499/46374
https://hdl.handle.net/11499/46374
Publikováno v:
Geoheritage. 12
Doğanay, Osman ( Aksaray, Yazar )
Zengibar Castle was built by the Isaurian during antique ages on the summit of Mount Asar, approximately 20 km west of the town of Bozkır, Konya, Turkey. The aims of this study are to determine the lithologica
Zengibar Castle was built by the Isaurian during antique ages on the summit of Mount Asar, approximately 20 km west of the town of Bozkır, Konya, Turkey. The aims of this study are to determine the lithologica