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Gold-sulphide disseminated mineralization of the Gadir deposit (Lesser Caucasus, Azerbaijan)

Abstract

The Gadir gold-sulfide deposit is located in the northwestern part of the Gedabek deposit in the Yogundag epithermal system. Ore-bearing strata are represented by Middle Jurassic volcanic and volcanic-sedimentary rocks formed under conditions of basalt-andesite-dacite-rhyolite volcanism formation. Mineralogy, gold mineralization, and metal content in the Gadir deposit have been investigated during ongoing studies to determine geological setting, temporal and spatial relationships with specific mineral assemblages and associations. Mine ralogy of ore bodies is mainly characterzed by pyrite, chalcopyrite, sphalerite, galena, magnetite, and native gold. Native gold was recorded in chalcopyrite that is probably related to the second stage of ore deposition.

About the Author

A. A. Bayramov
Azerbaijan State Oil and Industry University (ASOIU)
Russian Federation

PhD Student



References

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3. Bayramov, A. A. 2017: Geological Setting of The New Discovering Gadir Low Sulfidation Epithermal Deposit, Gedabek Ore District, Lesser Caucasus, Azerbaijan. IJISET – International Journal of Innovative Science, Engineering & Technology. 4. 12, 21–27.

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5. Novruzov, N., Valiyev, A., Bayramov, A., Mammadov, S., Ibrahimov, J., Ebdulrehimli, A. 2019: Mineral composition and paragenesis of altered and mineralized zones in the Gadir low sulfidation epithermal deposit (Lesser Caucasus, Azerbaijan). Iranian Journal of Earth Sciences. 11. 1. 14–29.

6. Veliyev, A., Bayramov, A., Ibrahimov, J., Mammadov, S., Alizhadeh, G. 2018: Geological Setting and Ore Perspective of the New Discovered Gadir Low Sulfidation Epithermal Deposit, Gedabek NW Flank, Lesser Caucasus, Azerbaijan. Universal Journal of Geoscience. 6. 3. 78–101. – DOI: 10.13189/ujg.2018.060304.


Review

For citations:


Bayramov A.A. Gold-sulphide disseminated mineralization of the Gadir deposit (Lesser Caucasus, Azerbaijan). Regional Geology and Metallogeny. 2020;(82):103–112. (In Russ.)

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ISSN 0869-7892 (Print)