Инд. авторы: Sukhorukov V.P., Savel'eva V.B., Jiang Y.D., Li Z.Y.
Заглавие: P-T path of metamorphism and U-Pb monazite and zircon age of the Kitoy terrane: Implication for Neoarchean collision in SW Siberian Craton
Библ. ссылка: Sukhorukov V.P., Savel'eva V.B., Jiang Y.D., Li Z.Y. P-T path of metamorphism and U-Pb monazite and zircon age of the Kitoy terrane: Implication for Neoarchean collision in SW Siberian Craton // Geoscience Frontiers. - 2020. - Vol.11. - Iss. 6. - P.1915-1934. - ISSN 1674-9871.
Внешние системы: DOI: 10.1016/j.gsf.2020.05.012; РИНЦ: 45368373; WoS: 000583042200002;
Реферат: eng: The first data on P-T metamorphic conditions coupled with U-Pb monazite and zircon age obtained for the Neoarchean Kitoy granulite-gneiss terrane (SW Siberian Craton). Alumina gneisses of the Kitoy terrane indicate two-staged metamorphic evolution. The first stage of regional metamorphism (M1) occurred at high-amphibolite facies conditions at T = 780-800 degrees C and P = 8-9 kbar. The second stage (M2) belongs to MT-HT/LP type of metamorphism with the wide temperature interval 600-750 degrees C and pressure 2-4 kbar. Two age peaks were established on the basis of U-Pb monazite and zircon dating in garnet-anthophyllite gneisses. Both of them correspond to the Neoarchean age: the age of M1 falls into the interval of ca. 2489-2496 Ma, the age of M2 - ca. 2446-2456 Ma. The high-temperature metamorphism of the Kitoy block and nearly coeval granitoid magmatism can be an evidence for the Neoarchean collision in SW Siberian craton.
Ключевые слова: MINERALS; GEOCHEMISTRY; ROCKS; GARNET; TRACE-ELEMENTS; THERMODYNAMIC MODEL; SILLIMANITE SCHIST DEPOSIT; BLOCK SHARYZHALGAI-UPLIFT; P-T path; Metamorphism; Kitoy terrane; Neoarchean; Siberian craton; ANGARA-KAN BLOCK; BIOTITE;
Издано: 2020
Физ. характеристика: с.1915-1934
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