About tectonic conditions of formation of the structure of skarn deposit in Primorsky region
Authors:
Abstract
The area of the deposit by structure belongs to the most tectonically complex area of Sikhote-Alin. The complexity of its structure is caused by multiple manifestation of folding, discontinuous and magmatic processes that took place almost continuously from the Upper Paleozoic to Paleogene inclusive .....
Область исследования:
(Archived) Without section
Funding:
None
References
- Velikiy A. S. Structures of ore fields. PH of LSU, 1961.
- Virovlyansky G. M. On tectonic conditions of dyke intrusion and ore formation. Sov. Geol. 50, 1956.
- Wolfson F. I. Structures of endogenous ore deposits. In the collection Basic Problems in the Doctrine of Magmatogenic Ore Deposits. PH of the AS USSR, 1955.
- Karyakin A. E. 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. Proc. IGS, 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. Proc. IGS, iss. 162, No. 17, 1955.
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