Vertical zonality of mineralization at the Nezhdaninskoye gold deposit
Abstract
The Nezhdaninskoye gold deposit is located in the northern part of the South Verkhoyansk synclinorium and is situated in the crestal part of the southern periclinal closure of the box-shaped Dyba anticline. The host rocks are represented by a monotonous sequence of sandy siltstones and shales of Lower Permian age.
Область исследования:
(Archived) Without section
Funding:
None
References
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- Gamyanin G. N., Soloviev V. I. Gold-ore formations of East Yakutia. Sb.: Stroenie zemnoi kory Yakutii i zakonomernosti razmeshcheniya poleznykh iskopaemykh . Nauka, 1969 (in Russian)
- Grigorieva O. A., Kvyatkovsky E. M. Highly sensitive double-arc method of spectral analysis for gold and some dispersed elements. Zapiski Gornogo Instituta, 1963, vol. XLV, issue 2 (in Russian)
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- Silichev M. K. Geological position and structural features of the Nezhdaninskoye gold deposit. Geol. rudn. mestorozhd. , 1970, No. 2 (in Russian)
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