U-Pb calcite geochronology, EPR, geochemistry, and C-O-Sr isotopes of ancient marbles in the İznik Region (Bursa-Türkiye)

Göster/ Aç
Erişim
info:eu-repo/semantics/openAccessTarih
2025Yazar
Aysal, NamıkKarslıoğlu, Özge
Erdem, Emre
Guillong, Marcel
Öngen, Sinan
Uysal, İbrahim
Kaygısız, Ersin
Yıldırım, İpek
Üst veri
Tüm öğe kaydını gösterKünye
AYSAL, Namık, Özge KARSLIOĞLU, Emre ERDEM, Marcel GUILLONG, Sinan ÖNGEN, İbrahim UYSAL, Ersin KAYGISIZ & İpek YILDIRIM. “U-Pb calcite geochronology, EPR, geochemistry, and C-O-Sr isotopes of ancient marbles in the İznik Region (Bursa-Türkiye)”. Turkish Journal of Earth Sciences, 34.5 (2025): 650- 668.Özet
The İznik city (ancient Nicaea), located east of Lake İznik (known as -“Bithynia” in ancient times), has been an important
political and cultural centre of Asia Minor since the Hellenistic period. Marbles produced in the quarries in the vicinity (Ömerli and
İnikli villages, Deliktaş-Sarıtaş hills) were used both in the construction of the walls and in many ancient works in the city. Approximately
eighteen ancient marble quarries producing grey and white marbles were investigated in the region. Petrography, EPR, XRD, C-O-Sr
isotope and whole rock geochemistry analyses were performed for characterization of the samples collected from the quarries for the
provenance studies. According to the new geochemistry and C-O-Sr isotope data, the limestones forming the marbles were deposited
in open sea-ocean environments. U-Pb calcite dating determined that the white marbles were 93.06 ± 8.55 Ma, while the grey marbles
were 94.84 ± 1.41 Ma and 88.03 ± 2.13 Ma (Upper Cretaceous: Cenomanian-Coniacian). These ages probably correspond to the
crystallization/metamorphism ages of the marbles. The new data set obtained with this study will contribute to the understanding of
the geological evolution of the region, and will help researchers to better understand the source region of some white and grey marbles
used in ancient buildings.


















