About On tectonic conditions of formation of the structure of skarn deposit in the Primorsky region
Authors:
Abstract
The area of the deposit in terms of structure belongs to the most tectonically complex area of the Sikhote‑Alin. The complexity of its structure is caused by multiple manifestations of folding, disjunctive and magmatic processes that took place almost continuously from the Upper Paleozoic to the Paleogene inclusive. ...
Область исследования:
(Archived) Without section
Funding:
None
References
- Velikiy A. S. Structures of ore fields. Izd-vo LGU, 1961.
- Virovlyansky G. M. On tectonic conditions of dyke intrusion and ore formation. Sov. geol., vol. 50, 1956.
- Wolfson F. I. Structures of endogenous ore deposits. V sb. Osnovnye problemy v uchenii o magmatogennykh rudnykh mestorozhdeniyakh. Izd-vo AN SSSR, 1955.
- Karyakin A. E., Smirnova V. A. Structures of crustaceous ore fields. Nedra, 1967.
- Lukin L. I., Kushnarev I. P., Chernyshev V. F. About recurrence of directions of equal-age fracture systems. Tr. IGN, vol. 162, No. 17, 1955.
- Tetyaev M. M. Tectonics of ore fields of vein type. Sov. geol., iss. 9, 1940.
- Rybalov B. L. About applicability of deformation ellipsoid in studying the structure of ore fields and deposits. Tr. IGN, iss. 162, No. 17, 1955.
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