Ore pillars of the Deputatskoye deposit
Authors:
Abstract
The ore bodies of the Deputatskoye deposit (northeastern Yakut ASSR) are mineralized fault zones of complex structure, less frequently — veins and zones of veinlet-disseminated mineralization cutting weakly dislocated shale‑sandstone sequences of the Upper Jurassic. The ore bodies are mainly confined to steeply dipping fractures and fracture shear zones of diagonal (northeastern and northwestern) and sub‑latitudinal trend.
Область исследования:
(Archived) Without section
Funding:
None
References
- Ivanov V. V. Mineralogical and geochemical features and tin-bearing of tin ore deposits of Yakutia. Nauka, 1964. (in Russian)
- Kallistov P. L. Variability of mineralization and density of observations during exploration and sampling. Sovetskaya geologiya, iss. 53, 1956. (in Russian)
- Korolev A. V., Shekhtman P. A. Structural conditions of location of postmagmatic ores. Nedra, 1965. (in Russian)
- Lir Yu. V. Tectonic Conditions of Ore Formation at the Deputatskoye Tin Ore Deposit. Zapiski Gornogo Instituta, vol. LV, iss. 2, 1968. (in Russian)
- Nekrasov I. Ya. Main features of mineralization of Deputatskoye tin ore deposit. Tr. In-ta geol. Yakut. fil. SO AN SSSR, No. 7, 1960. (in Russian)
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