Ore pillars of the deputy deposit
Authors:
Abstract
Ore bodies of the Deputatskoye deposit (north-east of the Yakut ASSR) are mineralized crushing zones of complex structure, less often - veins and zones of vein-embedded mineralization, cutting weakly dislocated shale-sandstone deposits of the Upper Jurassic. The ore bodies predominate in steeply dipping fractures and fracture zones of diagonal (northeastern and northwestern) and near-latitudinal direction.
Область исследования:
(Archived) Without section
References
- Ivanov V. V. Mineralogical and geochemical features and indienosity of tin ore deposits of Yakutia. Nauka, 1964.
- Kallistov P. L. Variability of mineralization and density of observations during exploration and sampling. “Soviet Geology”, v. 53, 1956.
- Korolev A. V. V., Shechtman P. A. Structural conditions of post-magmatic ore placement. Nedra, 1965.
- Lear Y. V. Tectonic Conditions of Ore Formation at the Deputatskoye Tin Ore Deposit. Journal of Mining Institute, vol. LV, iss. 2, 1968.
- Nekrasov I. Ya. Main features of mineralization of Deputatskoye tin ore deposit. Proc. Institute of Geology of the Yakut. Branch of the SB AS USSR, No. 7. 1960.
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