2019
DOI: 10.5800/gt-2019-10-2-0419
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Thermochronology and Mathematical Modeling of the Formation Dynamics of Rare‐metal‐granite Deposits of the Altai Collision System

Abstract: The article presents an event correlation of the Permian‐Triassic granites of the Altai collision system, which are associated with industrial ore deposits and occurrences (Mo‐W, Sn‐W, Li‐Ta‐Be). The multi‐system and multi‐mineral isotope datings of igneous rocks and ore bodies (U/Pb, Re/Os, Rb/Sr, Ar/Ar‐methods) suggest the postcollisional (intraplate) formation of ore‐magmatic systems (OMS), the duration of which depended on the crustmantle interaction and the rates of tectonic exposure of geoblocks to the u… Show more

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Cited by 7 publications
(1 citation statement)
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“…The Kalguty garnet-biotite granitoids identified in previous models of magmatism [6] rather belong to the Kunush complex [2,7]. The Kunush plagiogranites, which constitute a particular element in the magmatism of the Kalba area, have a collisional origin and host gold in the West Kalba zone or secondary rare-metal mineralization (Ta, Nb, Be, Sn, Li, W) in the Kalba-Narym zone [8,9]. Plagiogranites are gray equigranular medium-grained varieties consisting of 59-62% plagioclase, 26-28% quartz, and small amounts of feldspar (2-4%), biotite (6.5%), and accessories (amphibole, apatite, zircon, arsenopyrite, etc., 0.3-0.6% in total).…”
Section: Li-bearing Pegmatites Of the Kalba-narym Metallogenic Zone (...mentioning
confidence: 99%
“…The Kalguty garnet-biotite granitoids identified in previous models of magmatism [6] rather belong to the Kunush complex [2,7]. The Kunush plagiogranites, which constitute a particular element in the magmatism of the Kalba area, have a collisional origin and host gold in the West Kalba zone or secondary rare-metal mineralization (Ta, Nb, Be, Sn, Li, W) in the Kalba-Narym zone [8,9]. Plagiogranites are gray equigranular medium-grained varieties consisting of 59-62% plagioclase, 26-28% quartz, and small amounts of feldspar (2-4%), biotite (6.5%), and accessories (amphibole, apatite, zircon, arsenopyrite, etc., 0.3-0.6% in total).…”
Section: Li-bearing Pegmatites Of the Kalba-narym Metallogenic Zone (...mentioning
confidence: 99%