 | | Journal (article/letter/editorial) | | pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia A.N. Zavaritskii Institute of Geology and Geochemistry...Sciences, Pochtovyi per.7, Yekaterinburg, 620151, Russia Received 29 October 2010; accepted 5 April 2011...of the Yenisei Ridge, rocks near the thrusts in area of the Tatarka deep fault underwent the medium-pressure...798–802 Ma. The older metamorphic complexes (Angara, Mayakon, Teya, and Chapa areas) are interpreted to have...splay faults in the eastward direction (Garevka area). On a regional scale, this may result from collision |  | | Journal (article/letter/editorial) | | pr. Akademika Koptyuga 3, Novosibirsk, 630090 Russia e-mail: likh@uiggm.nsc.ru Received November 20...States, and the Kola Peninsula and Yenisei Range in Russia. The prograde transformations of andalusite into...(Kuzeevskaya member of the Kan Group); (2) sillimanite–biotite–garnet gneisses and pyroxene–garnet–cordierite...member of the Kan Group); and (3) amphibolites, biotite–muscovite gneisses, and marbles (Yenisei Group)...70° Siberian craton Western Siberian plate Chapa area 2 5.8–8.4 kbar/ 630–710°C 60° 3 1 Central Asian |  | Likhanov, I. I., Kozlov, P. S., Popov, N. V., Reverdatto, V. V., Vershinin, A. E. (2006) Collisional metamorphism as a result of thrusting in the Transangara region of the Yenisei Ridge. Doklady Earth Sciences, 411 (1) 1313-1317 doi:10.1134/s1028334x06080332 | Journal (article/letter/editorial) | | States, and the Kola Peninsula and Yenisei Ridge in Russia), where prograde transformation of andalusite into... pr. akademika Koptyuga 3, Novosibirsk, 630090 Russia; e-mail: likh@uiggm.nsc.ru b Zavaritsky Institute...Pochtovyi per. 7, Yekaterinburg, 620151 Russia three (Chapa, Mayakon, and Angara) areas composed of Paleoproterozoic...and Upper Riphean rocks (Fig. 1). The Chapa and Mayakon areas are located in the Central uplift between...the Ishimbino and Tatarka deep faults. The Angara area covers the junction of the Transangara structural |  | | Journal (article/letter/editorial) | | localized distribution of metamorphic zones in the area directly underlying thrust faults with a measured...Yenisey Ridge along regional deep faults (Angara, Mayakon, and Chapa areas) and by opposite movements in...in the zone of secondary splay faults (Garevka area). Keywords: collisional metamorphism; Fe- and Al-rich...complexes of the Central Angara terrane, mainly in the area of the Tatarka deep faults. From north to south...distinguished four typical localities (Chapa, Garevka, Mayakon, and Angara), in which rocks of Palaeo-Mesoproterozoic |  | | Journal (article/letter/editorial) | | located within the Central Angar terrain; the Angar area is located in the junction zone between Transangarian...structures and the Angaro–Kansk block (Fig. 1). The Angar area is located in the interfluves of Angara–Belokopytovka–Tatarka...phyllite of the Sukhoi Ridge Suite. In the studied area, these are predominantly phyllitic schist of the... Siberian Craton Western Siberian Plate Chapa area 5.8–8.4 kbar 630–710 °C 2 60° 3 1 Central Asian...Yenisei Ridge I 60° 60° Teya area 5.7–7.1 kbar 660–698 °C T A Mayakon area 4.5–6.7 kbar 560–600 ° C |  | | Journal (article/letter/editorial) | | of the Russian Academy of Sciences, Novosibirsk, Russia 2 Centre for Tectonics, Exploration and Resources...Sciences, 3 prosp. Akad. Koptyuga, Novosibirsk 630090, Russia. Email: likh@igm.nsc.ru Funding information state...Grambling, 1992; Grambling, 1981; Grambling & Wil- Mayakon deposits were confirmed with the reserves calculated...complex (curve 1, Mayakon area; curve 2, Polkan area; 3, Teya area; and 4, Chapa area) and in the Garevka...metamorphism for the Boehls Butte area (Idaho); Mt. Moosilauke area, New Hampshire; Rio Mora, Pikuris |  | | Journal (article/letter/editorial) | | Branch, Russian Academy of Sciences, Novosibirsk, Russia of the Teya and Sukhoy Pit Groups, which comprise...(1) Bt (biotite) + Ms (muscovite) + Chl (chlorite) + Qtz (quartz) + Pl (plagioclase) (biotite zone); (2)...and staurolite, (3) Ryazanov Fm. (PR1) Biotite–amphibole, biotite–garnet schist, marble, (4) Karpinskii...andalusite, (5) Malaya Garevka Sequence (PR1) biotite and biotite–amphibole plagiogneiss with interlayers of...metrical zonation with the successive development of biotite–garnet–staurolite–andalusite–sillimanite zones |  | | Book | | conference proceedings. It covers the entire research area of geology including, but not limited to, economic...Branch, Russian Academy of Sciences Novosibirsk, Russia Valentin S. Sheplev (Deceased) V.S. Sobolev Institute...Branch, Russian Academy of Sciences Novosibirsk, Russia Igor I. Likhanov V.S. Sobolev Institute of Geology...Branch, Russian Academy of Sciences Novosibirsk, Russia Vasiliy Yu. Kolobov V.S. Sobolev Institute of...Branch, Russian Academy of Sciences Novosibirsk, Russia Oleg P. Polyansky V.S. Sobolev Institute of Geology |
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