In the studied area, the ore are presented both by primary mineralizations which are composed of sulphide minerals and by
secondary mineralizations which are composed of oxide and carbonate minerals. In the primary mineralizations the main minerals are pyrite,
sphalerite and galena. Also there are pirrotite, arscnopyrite, chalcopyrite, argantite, pyrargirite, magnetite, fahlore, geocronite, freislebenite.
boumonite, marcasite, boulangerile, meneginite, skutlerudite, molybdenite, electrum, native Au and native Ag in minor ratios. In primary
ore, the common gangue minerals are quartz, calcite and dolomite. In minor ratios, there are barite, siderite, seriate, biotite, muscovite and
chlorite. The secondary minerals are smitsonite, anglesite, seruscite, hematite, lepidocrocite, amorph iron hydroxide, gothite, malachite,
azurite, hemimorphide and hydrozincite. The main mineralization which occurs within some representative minerals has been realized in
four period. These periods can be distinguished by the definite textural and structural features such as ex solution, inclusion, idiomorphism,
slit, metasomatose or by the appearance and absence of some minerals.
Birincil Dil | İngilizce |
---|---|
Konular | Mühendislik |
Bölüm | Makaleler |
Yazarlar | |
Yayımlanma Tarihi | 1 Mayıs 1991 |
Yayımlandığı Sayı | Yıl 1991 Cilt: 112 Sayı: 112 |
Copyright and Licence
The Bulletin of Mineral Research and Exploration keeps the Law on Intellectual and Artistic Works No: 5846. The Bulletin of Mineral Research and Exploration publishes the articles under the terms of “Creatice Common Attribution-NonCommercial-NoDerivs (CC-BY-NC-ND 4.0)” licence which allows to others to download your works and share them with others as long as they credit you, but they can’t change them in any way or use them commercially.
For further details;
https://creativecommons.org/licenses/?lang=en