Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Levent KARADENİZLİ"'
Autor:
Levent KARADENİZLİ, Gürol SEYİTOĞLU, Gerçek SARAÇ, Nizamettin KAZANCI, Şevket ŞEN, Yavuz HAKYEMEZ, Didem SAVAŞÇI
Publikováno v:
Bulletin of the Mineral Research and Exploration, Vol 126, Iss 126, Pp 50-50 (2003)
Çankırı-Çorum havzası, Orta Anadolu'da Tersiyer'de gelişen havzalardan birisidir ve Paleosen'den Pliyosen'e kadar önemli tortul birikimine sahip olmuştur. Bu çalışmada havzanın Erken- Orta Miyosen dönemindeki tektonik rejimi ve buna bağ
Externí odkaz:
https://doaj.org/article/c5cbdcd907154c849ee555c5eea76fc8
Publikováno v:
Journal of Paleontology
Journal of Paleontology, Paleontological Society, In press, pp.1-23. ⟨10.1017/jpa.2018.60⟩
Journal of Paleontology, Paleontological Society, In press, pp.1-23. ⟨10.1017/jpa.2018.60⟩
Three localities in the Çankırı Basin—Kale Tepe 1 (KT1), Kale Tepe 2 (KT2), and Mahmutlar—yielded reliably documented rodent and lagomorph assemblages. These are in the Akkaşdağı Formation, which covers large areas in the central and southe
Autor:
Gerçek Saraç, Cemal Tunoğlu, Funda Akgün, Alaettin Tuncer, Sevket Sen, Mine Sezgül Kayseri-Özer, Levent Karadenizli, Neşe Oyal
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology
Palaeogeography, Palaeoclimatology, Palaeoecology, 2017, 467, pp.16-36. ⟨10.1016/j.palaeo.2016.05.022⟩
Palaeogeography, Palaeoclimatology, Palaeoecology, 2017, 467, pp.16-36. ⟨10.1016/j.palaeo.2016.05.022⟩
Palaeoclimatic and palaeoenvironmental interpretations are reconstructed from the sedimentary sequences of the Late Oligocene and Miocene–Pliocene boundary in the Cankiri-Corum Basin based on evidence obtained from palynofloras and ostracod and mam
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7f369645282a26f71a37fbbf4ef6aea7
https://hal.science/hal-03893088
https://hal.science/hal-03893088
Autor:
Ozan Erdal, Levent Karadenizli, Yeşim Büyükmeriç, Sevket Sen, Grégoire Métais, Neşe Oyal, Ebru Albayrak, Pierre-Olivier Antoine, Gerçek Saraç
Publikováno v:
Palaeontologia Electronica
Palaeontologia Electronica, 2016, pp.19.3.37A. ⟨10.26879/629⟩
Palaeontologia Electronica, Coquina Press, 2016, pp.19.3.37A. ⟨10.26879/629⟩
Palaeontologia Electronica, 2016, pp.19.3.37A. ⟨10.26879/629⟩
Palaeontologia Electronica, Coquina Press, 2016, pp.19.3.37A. ⟨10.26879/629⟩
A new assemblage of ruminants from five distinct Oligocene localities of the Kizilirmak Formation, Central Anatolia, Turkey is described. The tragulids Iberomeryx parvus, and Iberomeryx sp. (large), as well as a probable large lophiomerycid have been
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::390f036ae3c6408b7859f176f3e5d3f9
https://hal.umontpellier.fr/hal-01922849/document
https://hal.umontpellier.fr/hal-01922849/document
In central eastern Anatolia which is located between Eurasia and Africa, the study of basin developments between late Eocene and early Miocene is of great importance for understanding the process of the closure of the Neo-Tethys Ocean and the formati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5b65b7258e06a7c3cdd49e05652f3df8
https://hdl.handle.net/20.500.12438/7256
https://hdl.handle.net/20.500.12438/7256
Autor:
Levent Karadenizli
Publikováno v:
Sedimentary Geology. 237:1-29
The Çankiri-Çorum Basin is one of the largest basins of Central Anatolia to have developed Oligocene to Quaternary terrestrial environments. The basin contains significant raw materials for industry and energy, but the determination of their distri
Publikováno v:
MorphoMuseum
MorphoMuseum, Association Palæovertebrata, 2015, 1 (2), ⟨10.18563/m3.1.2.e4⟩
MorphoMuseum, 2015, 1 (2), ⟨10.18563/m3.1.2.e4⟩
MorphoMuseum, Association Palæovertebrata, 2015, 1 (2), ⟨10.18563/m3.1.2.e4⟩
MorphoMuseum, 2015, 1 (2), ⟨10.18563/m3.1.2.e4⟩
International audience; 3D model related to the publication: Orliac M.J., Karadenizli L., Antoine P.-O., Sen S. 2015. Small hyotheriine suids (Mammalia, Artiodactyla) from the late early Miocene of Turkey and a short overview of early Miocene small s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f88064362f8583c95a2d927a30b58062
https://hal.archives-ouvertes.fr/hal-01904996
https://hal.archives-ouvertes.fr/hal-01904996
Publikováno v:
Palaeontologia Electronica
Palaeontologia Electronica, Coquina Press, 2015, 18 (2), pp.18.2.30A. ⟨10.26879/547⟩
Palaeontologia Electronica, 2015, 18 (2), pp.18.2.30A. ⟨10.26879/547⟩
Palaeontologia Electronica, Coquina Press, 2015, 18 (2), pp.18.2.30A
Palaeontologia Electronica, Coquina Press, 2015, 18 (2), pp.18.2.30A. ⟨10.26879/547⟩
Palaeontologia Electronica, 2015, 18 (2), pp.18.2.30A. ⟨10.26879/547⟩
Palaeontologia Electronica, Coquina Press, 2015, 18 (2), pp.18.2.30A
Suoids are conspicuous components of late early Miocene faunas in Europe, Asia, and Africa. Strikingly, despite a rich fossil record at the Old World scale, no early Miocene suoid remains were known thus far from Anatolia, a region located at the cro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::583ea7d9e827526069753662bec1c7c5
https://hal.sorbonne-universite.fr/hal-01275763/file/547.pdf
https://hal.sorbonne-universite.fr/hal-01275763/file/547.pdf
Publikováno v:
Carbonates and Evaporites. 17:197-209
The upper Miocene non-marine sediments of the Cankiri-Corum basin in central Anatolia, have both evaporitic and non-evaporitic successions. These sediments were deposited in an evaporitic lake which had temporary episodes of palustrine conditions in
Publikováno v:
Terra Nova. 12:245-251