Some features of primary zonation of mineralization in tin-polymetallic deposits
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Abstract
Many ore bodies of tin deposits of South-Eastern Primorye, characterized by insignificant depth of erosion cut, have a distinct vertical zonality, expressed in the replacement with depth of weakly tin-bearing essentially sulfide (polymetallic) mineral associations with low-sulfide cassiterite-bearing.
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References
- Lugov S.F., Makeev B.V., Potapova T.M. Regularities of formation and location of olozorodnye deposits of the North-East of the USSR. M., Nedra, 1972. 360 p.
- Pridatko M.R., Ananyin V.A. Geological Structure and Prospects of the Trudnenskoye Ore Field. - In the book: Materials on Geology and Mineral Resources of the North-East of the USSR. Magadan, Magadan Book Publishing House, 1980, vol. 25, p. 236-238.
- Radkevich E.A. Types of zonality of tin ore deposits. - In the book: Prediction of hidden mineralization on the basis of zonality of hydrothermal deposits. M., Nauka, 1976, p. 89-95.
- Chaikovsky V.K. Geology of tin-bearing deposits of the North-East of the USSR. Moscow, Gosgeoltekhizdat, 1960. 335 p.
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