About tectonic conditions of formation of the structure of skarn deposit in Primorsky region
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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 .....
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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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