The Upper Cretaceous (Upper Santonian-Campanian) successions were measured from two different basins of Turkey, Haymana basin and Mudurnu-Göynük basin. The measured Alagöz and Göynük sections are dominantly composed of red marly beds and fine grained siliciclastic green-gray beds with occasional interruption of fine grained turbiditic bedding. A variety of lithofacies are identified in the studied sections, including radiolarian packstone, silty marls, marls, mudstone, claystone, siltstone and fine grained quartzwacke sandstone. Abundant planktonic foraminifers and low presences of other microfossils are observed within the thin sections. The grains are mostly quartz with less percent of accessory minerals. The depositional environments are...
The stratigraphy of the uppermost levels of the Menderes Massif is controversial and within its deta...
The stratigraphy of the uppermost levels of the Menderes Massif is controversial and within its deta...
© 2014 Elsevier Ltd. A Cretaceous-Paleogene (K-Pg) succession is studied in detail in the Mudurnu-G...
The Haymana basin in Central Anatolia (Turkey) formed on a Late Cretaceous to Middle Eocene fore ar...
This study describes and interprets Upper Cretaceous volcaniclastics interbedded with hemipelagic to...
The study areas located near the towns of Goynok, Muclurnu and Nallihan in the central northwestern ...
Upper Cretaceous strata at Göynük, northwestern Anatolia, Turkey, provide a geological record of the...
The Santonian–Campanian boundary interval close to the village of Göynük in northwestern Turkey (Bol...
Upper Cretaceous strata exposed at Göynük (Mudurnu-Göynük basin, Bolu Province, Northwestern Anatoli...
A Cretaceous-Paleogene (K-Pg) succession is studied in detail in the Mudurnu-Goynuk basin in northwe...
A Cretaceous-Paleogene (K-Pg) succession is studied in detail in the Mudurnu-G\uf6yn\ufck basin in n...
A Cretaceous-Paleogene (K-Pg) succession is studied in detail in the Mudurnu-Göynük basin in northwe...
Upper Cretaceous strata at Goynuk, northwestern Anatolia, Turkey, provide a geological record of the...
The frontal belt of the southeastern Anatolia fold-thrust belt in Turkey contains several small to m...
The Montian Kartal Formation lies in the south-west of Ankara region and overlies the Upper Cretaceo...
The stratigraphy of the uppermost levels of the Menderes Massif is controversial and within its deta...
The stratigraphy of the uppermost levels of the Menderes Massif is controversial and within its deta...
© 2014 Elsevier Ltd. A Cretaceous-Paleogene (K-Pg) succession is studied in detail in the Mudurnu-G...
The Haymana basin in Central Anatolia (Turkey) formed on a Late Cretaceous to Middle Eocene fore ar...
This study describes and interprets Upper Cretaceous volcaniclastics interbedded with hemipelagic to...
The study areas located near the towns of Goynok, Muclurnu and Nallihan in the central northwestern ...
Upper Cretaceous strata at Göynük, northwestern Anatolia, Turkey, provide a geological record of the...
The Santonian–Campanian boundary interval close to the village of Göynük in northwestern Turkey (Bol...
Upper Cretaceous strata exposed at Göynük (Mudurnu-Göynük basin, Bolu Province, Northwestern Anatoli...
A Cretaceous-Paleogene (K-Pg) succession is studied in detail in the Mudurnu-Goynuk basin in northwe...
A Cretaceous-Paleogene (K-Pg) succession is studied in detail in the Mudurnu-G\uf6yn\ufck basin in n...
A Cretaceous-Paleogene (K-Pg) succession is studied in detail in the Mudurnu-Göynük basin in northwe...
Upper Cretaceous strata at Goynuk, northwestern Anatolia, Turkey, provide a geological record of the...
The frontal belt of the southeastern Anatolia fold-thrust belt in Turkey contains several small to m...
The Montian Kartal Formation lies in the south-west of Ankara region and overlies the Upper Cretaceo...
The stratigraphy of the uppermost levels of the Menderes Massif is controversial and within its deta...
The stratigraphy of the uppermost levels of the Menderes Massif is controversial and within its deta...
© 2014 Elsevier Ltd. A Cretaceous-Paleogene (K-Pg) succession is studied in detail in the Mudurnu-G...