Инд. авторы:	Mekhonoshin A.S., Ernst R., Soderlund U., Hamilton M.A., Kolotilina T.B., Izokh A.E., Polyakov G.V., Tolstykh N.D.
Заглавие:	Relationship between platinum-bearing ultramafic-mafic intrusions and large igneous provinces (exemplified by the Siberian Craton)
Библ. ссылка:	Mekhonoshin A.S., Ernst R., Soderlund U., Hamilton M.A., Kolotilina T.B., Izokh A.E., Polyakov G.V., Tolstykh N.D. Relationship between platinum-bearing ultramafic-mafic intrusions and large igneous provinces (exemplified by the Siberian Craton) // Russian Geology and Geophysics. - 2016. - Vol.57. - Iss. 5. - P.822-833. - ISSN 1068-7971. - EISSN 1878-030X.
Идентиф-ры:	DOI: 10.1016/j.rgg.2015.09.020; РИНЦ: 27154002; SCOPUS: 2-s2.0-84969776630; WoS: 000377370700014;
Реферат:	eng: This study aims at summarizing available geological and geochemical data on known Proterozoic platinum-bearing ultramafic-mafic massifs in the south of Siberia. Considering new data on geochemistry and geochronology of some intrusions, it was feasible to compare ore-bearing complexes of different time spans and areas and to follow their relationships with the recognized large igneous provinces. In the south of Siberia, the platinum-bearing massifs might be united into three age groups: Late Paleoproterozoic (e.g., Chiney complex, Malozadoisky massif), Late Mesoproterozoic (e.g., Srednecheremshansky massif), and Neoproterozoic (e.g., Kingash complex, Yoko-Dovyren massif, and massifs in the center of the East Sayan Mts.). In most massifs but Chiney the initial magmas are magnesium-rich. On paleogeodynamic reconstructions, the position of the studied massifs is the evidence that three most precisely dated events in North Canada continued into southern Siberia: In the period 1880-1865 Ma, it was the Ghost-Mara River-Morel LIP; at 1270-1260 Ma, the Mackenzie LIP; and at 725-720 Ma, Franklin LIP. In Siberia, the mostly productive massifs with respect to PGE-Ni-Cu mineralization are those linked with the Franklin LIP: Verkhny Kingash, Yoko-Dovyren, and central part of the Eastern Sayan Mountains, e.g., Tartay, Zhelos, and Tokty-Oy. © 2015.
Ключевые слова:	PGE-Ni-Cu deposits; Mafic-ultramafic intrusions; Large igneous provinces;
Издано:	2016
Физ. хар-ка:	с.822-833
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