Mineralogical, geochemical, and gemological characteristics of silicic gemstone in Aydıncık (Yozgat-Turkey)
Yazarlar (1)
Doç. Dr. Zeynel BAŞIBÜYÜK Kırşehir Ahi Evran Üniversitesi, Türkiye
| Makale Türü | Özgün Makale (SSCI, AHCI, SCI, SCI-Exp dergilerinde yayınlanan tam makale) | ||
| Dergi Adı | Arabian Journal of Geosciences (Q4) | ||
| Dergi ISSN | 1866-7511 Wos Dergi Scopus Dergi | ||
| Dergi Tarandığı Indeksler | SCI-Expanded | ||
| Makale Dili | İngilizce | Basım Tarihi | 06-2018 |
| Cilt / Sayı / Sayfa | 11 / 12 / 1–11 | DOI | 10.1007/s12517-018-3615-2 |
| Makale Linki | http://dx.doi.org/10.1007/s12517-018-3615-2 | ||
| Özet |
| There are chalcedony and amethyst formations in two fields in Aydıncık-Yozgat (West of Aydıncık District, Keşlik area and Southwestern of Hacıilyas). The gemstones in this region have been formed within the gaps and cracks of the brecciated rocks of the fault zone in altered andesites. Chalcedony and amethyst are either present in the form of crack fillings from a few millimeters to 10 cm in width, or in the form of generally oval pore fillings reaching a few centimeters to 40 cm in diameter. The chalcedony is composed of 0.1-mm–centimeter-thick bands parallel to each other in varying tones ranging from light blue/white to dark blue to reddish brown, and in some points in the central part of this banded structure are large crystalline quartz and amethysts. Chalcedony occurs as kidney—banded and geodesic forms as cryptocrystalline and macrocrystalline. The altered volcanic rock with brecciated texture, which hosts … |
| Anahtar Kelimeler |
| Amethyst | Chalcedony | Gemology | Gemstone | Geochemistry |
BM Sürdürülebilir Kalkınma Amaçları
| Atıf Sayıları | |
| Google Scholar | 14 |
| Scopus | 10 |
| Web of Science | 8 |