| Makale Türü | Özgün Makale (SSCI, AHCI, SCI, SCI-Exp dergilerinde yayınlanan tam makale) | ||
| Dergi Adı | Geochemistry (Q2) | ||
| Dergi ISSN | 0009-2819 Wos Dergi Scopus Dergi | ||
| Dergi Tarandığı Indeksler | SCI-Expanded | ||
| Makale Dili | Türkçe | Basım Tarihi | 11-2024 |
| Cilt / Sayı / Sayfa | 84 / 4 / 126121–0 | DOI | 10.1016/j.chemer.2024.126121 |
| Makale Linki | https://doi.org/10.1016/j.chemer.2024.126121 | ||
| Özet |
| The study area located at the periphery of the collision zone between the Eurasian plate (i.e. Pontides) and Tauride-Anatolide platform, NE of Sivas in the east-central Turkey, which is part of the Tethyan Metallogenic Belt. Mixed-layer illite-smectite (Isingle bondS) and illite minerals are derived within the hydrothermal alteration zones with a few km2 surface areas (up to 30 km2) in Eocene volcanic and plutonic rocks. The representative Isingle bondS and illite samples taken from plutonic- and volcanic-hosted alteration zones are investigated by optical and scanning electron microscopy (SEM), X-ray diffraction (XRD), major and trace elements and Osingle bondH isotope geochemistry and Ksingle bondAr dating methods. Different types of hydrothermal alterations, such as propylitic and phyllic alteration in the plutonic rocks and argillic alteration in the volcanic rocks were developed as a result of intrusion of Kösedağ … |
| Anahtar Kelimeler |
| Clay minerals | Eocene magmatism | Hydrothermal alteration | K-Ar dating | Stable isotope geochemistry |
| Atıf Sayıları | |
| Google Scholar | 2 |
| Scopus | 2 |
| Web of Science | 2 |
| Dergi Adı | Geochemistry |
| Yayıncı | Elsevier GmbH |
| Açık Erişim | Hayır |
| ISSN | 0009-2819 |
| E-ISSN | 1611-5864 |
| CiteScore | 4,5 |
| SJR | 0,729 |
| SNIP | 0,998 |