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
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- 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.
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