Research Article
Year 1987,
, 0 - 0, 01.01.1987
Abstract
References
- Ankara Üniversitesi – Communications Faculty of Sciences University of Ankara Series C Biology Dergisi
Year 1987,
, 0 - 0, 01.01.1987
Abstract
Tbe Bakacak ore consist of Pb-Zn and Pb-Zn«Cu veins. These veins represent essentîally kata and meso-thennal zones and in some cases reach to the hottest pârts of the epi-thermal zone.
In the paragenesis enargite and uraninite are present which represent typical minerals of the hydrothermal origin. The uraninite is reported for the first time in the Bakacak ore deposit during th is researeh. Quartz, amethyst and calcite are the majör gangue minerals. The hydrot hermal Solutions which lead to the formatin of ore veins also cause intensive alteration of the waU rock.
Keywords
References
- Ankara Üniversitesi – Communications Faculty of Sciences University of Ankara Series C Biology Dergisi
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Details
| Primary Language | English |
|---|---|
| Subjects | Structural Biology |
| Journal Section | Research Articles |
| Authors | |
| Publication Date | January 1, 1987 |
| Published in Issue | Year 1987 |
Communications Faculty of Sciences University of Ankara Series C-Biology.
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