Özet
The Kirazlıyayla deposit is one of Pb-Zn (±Cu) deposits associated with andesitic volcanism cutting through the metamophics of Karakaya complex. It is a structurally controlled, vein-stockwork style, mesothermal ore deposit. Replacement, brecciation, vein/veinlets, carries, sea-island, and dissemination textures were identified. Pyrite, sphalerite, chalcopyrite, galena, tennantite, and covellite constitute the ore mineral paragenesis. Quartz, calcite and dolomite with kaolinite account for the gangue minerals. Supergene stage is insignificant. The Kirazlıyayla mineralization is a Zn-Pb (±Cu) mineralization hosted by tectonically controlled andesitic volcanism within the Karakaya metamorphics and has common features with the other occurrences in the western Anatolia.
| Orijinal dil | İngilizce |
|---|---|
| Ana bilgisayar yayını başlığı | Springer Proceedings in Earth and Environmental Sciences |
| Yayınlayan | Springer Nature |
| Sayfalar | 84-89 |
| Sayfa sayısı | 6 |
| DOI'lar | |
| Yayın durumu | Yayınlandı - 2019 |
| Harici olarak yayınlandı | Evet |
Yayın serisi
| Adı | Springer Proceedings in Earth and Environmental Sciences |
|---|---|
| ISSN (Basılı) | 2524-342X |
| ISSN (Elektronik) | 2524-3438 |
Bibliyografik not
Publisher Copyright:© 2019, The Author(s).
Finansman
The authors would like to acknowledge support received from Meyra Mining company for their courteous support during the field work.
| Finansörler | Finansör numarası |
|---|---|
| Meyra Mining |