Stratigraphy of Upper Cretaceous-paleogene sequences in the Southern and Eastern Menderes Massif (Western Turkey)

• Main Authors: Ozer, S., SARI, BİLAL, Toker, V., Özkar, I., SÖZBİLİR, HASAN
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2001
• Subjects: Planktonic foraminifera
• Online Access: https://avesis.deu.edu.tr/publication/details/9155ff1e-83fd-4f13-a221-bb60635bc24c/oai

The stratigraphy of the uppermost levels of the Menderes Massif is controversial and within its details lie vital constraints to the tectonic evolution of south-western Turkey. Our primary study was carried out in four reference areas along the southern and eastern Menderes Massif. These areas lie in the upper part of the Menderes metamorphic cover and have a clear stratigraphic relationship and contain datable fossils. The first one, in the Akbük-Milas area, is located south-east of Bafa Lake where the Milas, then Kizilaǧaç and Kazikli formations are well exposed. There, the Milas formation grades upwards into the Kizilaǧaç formation. The contact between the Kizilaǧaç and the overlying Kazikli formation is not clearly seen but is interpreted as an unconformity. The Milas and Kizilaǧaç formations are also found north of Muǧla, in the region of Yataǧan and Kavaklidere. In these areas, the Milas formation consists of schists and conformably overlying platform-type, emery and rudist-bearing marbles. Rudists form the main palaeontological data from which a Santonian-Campanian age is indicated. The Kizilaǧaç formation is characterized by reddish-greyish pelagic marbles with marly-pelitic interlayers and coarsening up debris flow deposits. Pelagic marbles within the formation contain planktonic foraminifera and nanoplankton of late Campanian to late Maastrichtian age. The Kazikli formation is of flysch type and includes carbonate blocks. Planktonic foraminifera of Middle Palaeocene age are present in carbonate lenses within the formation. In the Serinhisar-Tavas area, Mesozoic platform-type marbles (Yilanli formation) belonging to the cover series of the Menderes Massif exhibit an imbricated internal structure. Two rudist levels can be distinguished in the uppermost part of the formation: the first indicates a middle-late Cenomanian age and the upper one is Santonian to Campanian in age. These marbles are uncomformably covered by the Palaeocene-Early Eocene Zeybekölentepe formation with polygenetic breccias. In the ...