Инд. авторы:	Doroshkevich A.G., Chebotarev D.A., Sharygin V.V., Prokopyev I.R, Nikolenko A.M.
Заглавие:	Petrology of alkaline silicate rocks and carbonatites of the Chuktukon massif, Chadobets upland, Russia: Sources, evolution and relation to the Triassic Siberian LIP
Библ. ссылка:	Doroshkevich A.G., Chebotarev D.A., Sharygin V.V., Prokopyev I.R, Nikolenko A.M. Petrology of alkaline silicate rocks and carbonatites of the Chuktukon massif, Chadobets upland, Russia: Sources, evolution and relation to the Triassic Siberian LIP // Lithos. - 2019. - Vol.332-333. - P.245-260.
Идентиф-ры:	DOI: 10.1016/j.lithos.2019.03.006; РИНЦ: 38692431; SCOPUS: 2-s2.0-85062822336; WoS: 000464891900016;
Реферат:	eng: The petrogenesis of temporally and spatially associated carbonatitic and deeply derived carbonated alkaline silicate magmas provides an opportunity to gain insights into the nature of the deepest lithospheric mantle. The Chuktukon massif, which is part of the Chadobets alkaline ultramafic carbonatite complex (Chadobets upland, Siberian craton) is a carbonatite-melilitite-damtjernite intrusion, whose emplacement was coeval with the Siberian Traps large igneous province (LIP). In this study, the sources of the primary melts are examined, the petrogenetic evolution of the complex is reconstructed and the relationship with the Siberian LIP is also discussed. Isotopic and geochemical information indicate that the source for the Chuktukon primary melts was isotopically moderately depleted and the primary melts were formed by low degree partial melting of garnet carbonated peridotite. Hydrothermal processes caused O-18- and C-13- enrichment. The weathering process was accompanied by trace element re-distribution and enrichment of the weathering crust in Zn, Th, U, Nb, Pb and REE, relative to the Chuktukon rocks and a change in radiogenic (Sr, Nd) isotope compositions. (C) 2019 Elsevier B.V. All rights reserved.
Ключевые слова:	DOLOMITE CARBONATITE; ISOTOPIC COMPOSITIONS; GULI MASSIF; TRACE-ELEMENT; MELT INCLUSIONS; LIQUID IMMISCIBILITY; FLOOD BASALTS; IGNEOUS PROVINCE EVIDENCE; OLDOINYO LENGAI VOLCANO; Source characteristics; Triassic Siberian LIP; Chadobets upland; Carbonatites; Damtjernites; Melilitites; NORTH TRANSBAIKALIA;
Издано:	2019
Физ. хар-ка:	с.245-260