Research Article
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Year 1987, Volume: 05 (1987) , 0 - 0, 01.01.1987
https://doi.org/10.1501/Commuc_0000000123

Abstract

References

  • Ankara Üniversitesi – Communications Faculty of Sciences University of Ankara Series C Biology Dergisi

THE ORE MICROSCOPIC INVESTIGATION OF THE BAKACAK (ORDU) PB-ZN-CU-ORE DEPOSİT

Year 1987, Volume: 05 (1987) , 0 - 0, 01.01.1987
https://doi.org/10.1501/Commuc_0000000123

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.

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

Şükrü Koç This is me

Publication Date January 1, 1987
Published in Issue Year 1987 Volume: 05 (1987)

Cite

Communications Faculty of Sciences University of Ankara Series C-Biology.

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