| | Journal (article/letter/editorial) | regional metamorphism of VMS ores varies from prehnite-pumpellyite facies (t = 150300°C, P = 0.5-4 kbar)...pseudomonoclinal steeply-dipping vein-like bodies (Karabash district). The massive sulphide transformation in PTX-gradient...in relation to the geodynamic evolution of the region, as well as the NU interpretation of their geochemical...volcano-sedimentary rocks mostly limited to the prehnite-pumpellyite facies, much lower than deposits of...metamorphosed VMS deposits of the Krasnouralsk ore district are arranged along the eastern margin of the Tagil | | Maslennikov, V.V., Ayupova, N.R., Herrington, R.J., Danyushevskiy, L.V., Large, R.R. (2012) Ferruginous and manganiferous haloes around massive sulphide deposits of the Urals. Ore Geology Reviews, 47. 5-41 doi:10.1016/j.oregeorev.2012.03.008 | Journal (article/letter/editorial) | these zones to south are known as the West Mugodjar region, where basal sequences are dominated by basalts...Aidyrlya (Aidyrlya), 29 — Sredneorsk (Priorskoye, 50 Let Oktyabrya), 30 — Verkhne-Orsk (Limannoye), 31 — Berchogur...the Shemoor group of VMS deposits in the Ivdel district (see Fig. 2 (column II). The magnetite-pyrite...the Karpinsk district (see Fig. 3). Thin (2 m) hematitic chert has been traced up to 50 m from the ore...sediments Deposits of the Urals Deposits of other region Basalt Chert, jasper, jasperite Fe-moderate |
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