Silicified Woods Consist with Malachite, Azurite, and Hematite in the Middle Eocene Çekerek Formation, Tokat—Turkey
Yazarlar (3)
Dr. Öğr. Üyesi İlkay KAYDU AKBUDAK Kırşehir Ahi Evran Üniversitesi, Türkiye
Doç. Dr. Zeynel BAŞIBÜYÜK Kırşehir Ahi Evran Üniversitesi, Türkiye
Meltem Gürbüz Mersin Üniversitesi, Türkiye
| Makale Türü | Özgün Makale (SSCI, AHCI, SCI, SCI-Exp dergilerinde yayınlanan tam makale) | ||
| Dergi Adı | Lithology and Mineral Resources (Q4) | ||
| Dergi ISSN | 0024-4902 Wos Dergi Scopus Dergi | ||
| Dergi Tarandığı Indeksler | SCI-Expanded | ||
| Makale Dili | Türkçe | Basım Tarihi | 11-2021 |
| Cilt / Sayı / Sayfa | 56 / 6 / 548–558 | DOI | 10.1134/S002449022106002X |
| Makale Linki | http://dx.doi.org/10.1134/s002449022106002x | ||
| Özet |
| In the vicinity of Yücepinar Village of Zile district of Tokat province, there are silicified wood formations in agglomerate levels in the Çekerek formation Middle Eocene aged. These formations consist of well— preserved tree trunks of about 1.5 m in diameter or branches and trunk parts in mm—1 m length. Generally, they are open-brownish cream; in some places they demonstrate dark brown, green, and blue colors. According to XRD and FT-IR analysis results of the samples, it is determined that the silicified wood formations are composed of quartz, cristobalite, malachite, azurite, hematite, graphite, and goethite minerals. According to XRF and ICP-MS analyzes of silicified woods, the high iron content (Fe2O3 8.29–63.79%) in the samples causes red brown color while the increase in copper content (Cu >10 000 ppm) causes blue and green colors. As a result of the cabochon cuts made from the silicified wood … |
| Anahtar Kelimeler |
| silicified wood | azurite | malachite | mineralogy | geochemistry |
BM Sürdürülebilir Kalkınma Amaçları
| Atıf Sayıları | |
| WoS | 5 |
| SCOPUS | 4 |
| Google Scholar | 11 |