Automated Author ProfileÖzge, Karslıoğlu
İstanbul University-Cerrahpasa0000-0003-3203-6756
Özge, Karslıoğlu
Current S-Index
Sum of Dataset Indices for all datasets
Average Dataset Index per Dataset
Average Dataset Index per dataset
Total Datasets
Total datasets for this author
Average FAIR Score
Average FAIR Score per dataset
Total Citations
Total citations to the author's datasets
Total Mentions
Total mentions of the author's datasets
S-Index Interpretation
The S-Index (Sharing Index) is a comprehensive metric that represents the cumulative impact of all your datasets. It is calculated as the sum of Dataset Index scores across all your claimed datasets.
What it means:
- A higher S-index indicates greater overall impact of your datasets relative to typical datasets in their fields of research
- The S-Index grows as you add more datasets or as existing datasets gain more citations and mentions
- It provides a single number to track your research data impact over time
Current S-Index: 1.8 (sum of 1 dataset Dataset Index scores)
More information here.
S-Index Over Time
Cumulative Citations Over Time
Cumulative Mentions Over Time
Datasets
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.
Authors
- Namık, Aysal ;
- Özge, Karslıoğlu ;
- Emre, Erdem ;
- Marcel, Guillong ;
- Sinan, Öngen ;
- Tonguç, Uysal ;
- Ersin, Kaygısız ;
- Yıldırım İpek Deniz