Titlebook: Geology and Metallogeny of Copper Deposits; Proceedings of the C Günther H. Friedrich,Alexandr D. Genkin,Frank M. V Conference proceedings

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Application of Stable Isotopic Studies to Problems of Magmatic Sulfide Ore Genesis With Special Refey continental crust material. Partial melting and devolatilization of country rocks are important processes in the generation of many Cu—Ni deposits associated with mafic igneous rocks. Sulfur isotopes provide a means of evaluating the possibility of extraneous sulfur addition to a melt. Variability

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Controls on the Formation of Komatiite-Associated Nickel-Copper Sulfide Deposits and ore distribution: (1) stratiform, massive-matrix-disseminated sulfides hosted by cumulate komatiite lava flows (lava conduits), or strata-bound, coarse disseminated sulfides hosted by cumulate komatiite bodies near volcanic vents, and (2) strata-bound, finely disseminated sulfides and more rest

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Depositional Environments of Volcanic Peridotite-Associated Nickel Sulphide Deposits with Special Rehe distribution of individual ore shoots. Although considerably modified by tectonism and amphibolite facies metamorphism, there are distinctive stratigraphic relationships within the host ultramafic komatiite sequence that distinguish ore environments from adjacent areas barren of Fe—Ni sulphides..

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Sulfide Petrology and Genesis of Copper-Nickel Ore Depositsr with the deposits of greenstone belts and some others, are classified as the deposits connected with ore-bearing volcanic-intrusive complexes of intercontinental rift zones. Massive sulfide ores, sulfide-bearing intrusions, and ultramafic volcanites are shown to have been formed as the result of s

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Types and Distinctive Features of Ore-Bearing Formations of Copper-Nickel Depositsrite formation; (3) Bushveld and Monchegorsk-type gabbro-norite-pyroxenite-peri- dotite formation; (4) Pechenga-type gabbro-pyroxenite-peridotite formation; (5) Kambalda- and Aliarechensk-type pyroxenite-peridotite formation; (6) Mount- keith-type peridotite-dunite; and (7) regenerated Subdury-type

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On the Role of Metamorphism in the Formation of Nickel-Copper Sulfide Deposits in the Kola Peninsulagmatic stage, syngenetic ores are simple and constant in the composition formed. In the regional metamorphic stage, epigenetic ores appear that are distinguished by diversities in mineral composition, typical of the specific tectonic zones formed during such metamorphism. Late metamorphic alteration

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