Abstract
These deposits and those of greenstone belts and others are classified as the deposits connected with ore-bearing volcanic-intrusive complexes of intercontinental rift zones. They are shown to have formed by successive emplacements of magmatic melts produced during differentiation of mantle magmas. Distribution zonality and formation conditions are discussed. -R.E.S.
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CITATION STYLE
APA
Distler, V. V., Genkin, A. D., & Dyuzhikov, O. A. (1986). Sulphide petrology and genesis of copper-nickel ore deposits. Geology and Metallogeny of Copper Deposits, 111–123. https://doi.org/10.1007/978-3-642-70902-9_7
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