Abstract
Variations in mineralogy and compositions of principal rock-forming minerals serve as an indicator of basaltic magma differentiation. Features of the composition of olivine, pyroxenes, plagioclase, spinel group minerals, micas, and ilmenite are described in Sect. 4.1. The compositions of olivine and plagioclase in layered intrusions vary from forsterite to fayalite and from albite to anorthite, respectively. Pyroxene is present as augite of the varying composition; pigeonite and orthopyroxene are less abundant. Minerals of the spinel group are represented by a series of spinel, chromite, and magnetite. Chromespinellides form accessory impregnations and accumulations in gabbrodolerites and pegmatoids. Micas occur as phlogopite–annite with the Fe/(Fe + Mg) ratio ranging from 1 to 90 at%.
In Sect. 4.2, features of the geochemistry of Cr, PGE, Ni, Ti, and S in basalts, barren, and ore-bearing intrusions with the different degree of differentiation are described. Features of the PGE and Cr distribution in sequences of ore-bearing horizons and in various rock types are considered. In the geochemistry of nickel, the main attention is drawn to its distribution in rocks and minerals, as well as to behavior of nickel in the process of sulfide formation. The Ti content in traps and its variations in the sequences of layered intrusions depend on the initial composition of a basaltic melt and the extent of its differentiation. In the geochemistry of S, the main attention is drawn to the sulfur isotopic composition in sulfides and sulfates of the Talnakhsky ore junction.
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Ryabov, V.V., Shevko, A.Y., Gora, M.P. (2014). Mineralogy and Geochemistry of Traps. In: Trap Magmatism and Ore Formation in the Siberian Noril'sk Region. Modern Approaches in Solid Earth Sciences, vol 3. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-5022-7_4
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