 | Kislov, Evgeniy V., Erokhin, Yuriy V., Popov, Mikhail P., Nikolayev, Anatoliy G. (2021) Nephrite of Bazhenovskoye Chrysotile–Asbestos Deposit, Middle Urals: Localization, Mineral Composition and Color. Minerals, 11 (11) 1227 doi:10.3390/min11111227 | Journal (article/letter/editorial) | | Russian Academy of Sciences, 670047 Ulan-Ude, Russia Zavaritsky Institute of Geology and Geochemistry...Russian Academy of Sciences, 620016 Yekaterinburg, Russia; erokhin-yu@yandex.ru (Y.V.E.); popovm1@yandex...State Mining University, 620144 Yekaterinburg, Russia Institute of Geology and Oil and Gas Technologies...(Volga Region) Federal University, 420008 Kazan, Russia; anatolij-nikolaev@yandex.ru Correspondence: evg-kislov@ya...serpentinite type were found on the contact of after gabbro rodingites and serpentinites. The color is uniform |  | Palyanova, Galina, Murzin, Valery, Borovikov, Andrey, Karmanov, Nikolay, Kuznetsov, Sergei (2021) Native Gold in the Chudnoe Au-Pd-REE Deposit (Subpolar Urals, Russia): Composition, Minerals in Intergrowth and Genesis. Minerals, 11 (5) 451 doi:10.3390/min11050451 | Journal (article/letter/editorial) | | the Chudnoe Au-Pd-REE Deposit (Subpolar Urals, Russia): Composition, Minerals in Intergrowth and Genesis...the Chudnoe Au-Pd-REE Deposit (Subpolar Urals, Russia): Composition, Minerals in Intergrowth and Genesis...Akademika Koptyuga Pr., 3, 630090 Novosibirsk, Russia; borovikov.57@mail.ru (A.B.); krm@igm.nsc.ru (N...University, Pirogova Str., 2, 630090 Novosibirsk, Russia Zavaritsky Institute of Geology and Geochemistry...Akademika Vonsovskogo Str., 15, 620016 Ekaterinburg, Russia; murzin@igg.uran.ru Komi Science Center, Institute |  | | Journal (article/letter/editorial) | | of low-temperature Alpine-type serpentinized ultramafic T rocks (Salem et al., 2012; Surour, 2017)...with ~12% H2O (Mével, 2003). Metasomatism of ultramafic rocks AN continues from sea-floor serpentinization...all of the studied areas (Fig. 1), ophiolitic ultramafic rocks are mostly serpentinites that occurs as...ones, are useful for petrogenesis of mafic and ultramafic rocks in opholites. T Both rodingites and unrodingitized...serpentinite host (Table 6). At the contact with the ultramafic host, clinopyroxene is US more enriched in |
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