Rock Magnetic Studies of The Early Jurassic Middle Eocene Volcanic and Sedimentary Rocks of the Eastern Pontides
- 1Istanbul Technical University, Faculty of Mines, Department of Geophysical Engineering, Istanbul, Türkiye
- 2Gümüşhane University, Department of Mining and Mineral Extraction, Gümüşhane, Türkiye
- 3Gümüşhane University, Department of Geological Engineering, Gümüşhane, Türkiye
- 4Istanbul University-Cerrahpaşa, Department of Geophysical Engineering, Istanbul, Türkiye
In this research, we revealed the findings from rock magnetic analyses, including Isothermal Remanent Magnetization (IRM) and High-Temperature Susceptibility (HTS), conducted on various volcanic and sedimentary rocks from the Early Jurassic – Middle Eocene located in the Eastern Pontides. These magnetic studies offer valuable insights into the minerals causing magnetization, as well as the composition and changes in magnetic minerals within these rocks. The experiments were carried out at the Doç.Dr. Yılmaz İspir Paleomagnetism Laboratory, Istanbul University-Cerrahpaşa.
For the Isothermal Remanent Magnetization (IRM) studies, samples were collected from 57 sites in the Eastern Pontides, ensuring representation of each rock type. The analysis revealed that “Hematite”, “Magnetite”, and a combination of “Hematite + Magnetite” are the minerals responsible for magnetization in the selected samples. Moreover, it was discovered that in 41 out of the 57 sites, the samples reached saturation magnetization, indicating that "Magnetite" is the predominant mineral responsible for magnetization. The magnetic susceptibility of the rocks was examined during the heating and cooling stages in these high-temperature susceptibility measurements. High-temperature susceptibility measurements were used to assess whether the minerals responsible for magnetization in the rocks underwent any changes due to temperature, to determine the Curie temperatures, and to understand the domain structure. For this aspect of the study, 23 sites representing various ages and types of rocks were chosen for high-temperature susceptibility studies. It can be said that some rocks are rich in "Ti-Magnetite". It is observed that mineral phase transformation occurs in some rocks as a result of heating phases.
This study was supported by the project of the Scientific Research Projects Commission of Gümüşhane University with Project Number: 21.B0126.01.01.
How to cite: Algur, B. S., Kayın, S., Dokuz, A., Hisarlı, Z. M., and İşseven, T.: Rock Magnetic Studies of The Early Jurassic Middle Eocene Volcanic and Sedimentary Rocks of the Eastern Pontides, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-15097, https://doi.org/10.5194/egusphere-egu24-15097, 2024.
