SM-ND ISOTOPIC SYSTEMATICS OF ALKALINE ROCKS AND CARBONATITES FROM THE EDEL'VEIS COMPLEX, NORTHERN CHUYA RANGE, GORNYI ALTAI

dc.contributor.authorVrublevskii V.V.
dc.contributor.authorGertner I.F.
dc.contributor.authorRikhvanov L.P.
dc.contributor.authorZhuravlev D.Z.
dc.contributor.authorKrupchatnikov V.I.
dc.contributor.authorVladimirov A.G.
dc.date.accessioned2022-07-25T04:36:20Z
dc.date.available2022-07-25T04:36:20Z
dc.date.issued2004
dc.description.abstractThe obtained isotopic data suggest the following conclusions: alkaline rocks and carbonatites of the Edel'veis Complex formed at the late collisional stage in the Middle Ordovician; the comagmatic association was derived from moderately depleted PREMA-type mantle; and evolution of derivative melts was complicated by crustal contamination, which was responsible for increase in Sr, O, and C isotopic ratios in rocks and minerals.
dc.identifierhttps://www.elibrary.ru/item.asp?id=13460196
dc.identifier.citationDoklady Earth Sciences, 2004, 397, 6, 870-874
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/38359
dc.titleSM-ND ISOTOPIC SYSTEMATICS OF ALKALINE ROCKS AND CARBONATITES FROM THE EDEL'VEIS COMPLEX, NORTHERN CHUYA RANGE, GORNYI ALTAI
dc.typeСтатья

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