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S. I. Kostrovitsky

Researcher at Russian Academy of Sciences

Publications -  24
Citations -  330

S. I. Kostrovitsky is an academic researcher from Russian Academy of Sciences. The author has contributed to research in topics: Kimberlite & Craton. The author has an hindex of 7, co-authored 21 publications receiving 256 citations.

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Repeated kimberlite magmatism beneath Yakutia and its relationship to Siberian flood volcanism: Insights from in situ U–Pb and Sr–Nd perovskite isotope analysis

TL;DR: In this paper, the authors report combined ages and isotope compositions of perovskites from 50 kimberlite occurrences, sampled from 9 fields across the Yakutian kimbersite province on the Siberian craton, and suggest that kimbles formed repeatedly during at least 4 episodes: Late Silurian-Early Devonian (419-410 Ma), Late Devonian-Early Carboniferous (376-347 Ma), late Triassic (231-215 Ma), and Middle/Late Jurassic (171-156 Ma).
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Isotope-geochemical systematics of kimberlites and related rocks from the Siberian Platform

TL;DR: Using the ICP-MS method, a representative collection of kimberlites and related rocks from the Siberian Platform has been studied in this paper using the isotope systematics of Sr and Nd as well as trace element composition.
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Mantle sources of kimberlites through time: A U-Pb and Lu-Hf isotope study of zircon megacrysts from the Siberian diamond fields

TL;DR: In this paper, a comprehensive, internally consistent U-Pb and Lu-Hf isotope data set for 93 mantle-derived zircons from the Yakutian kimberlite province confirms and further refines the four major episodes of kimitic magmatism on the Siberian craton: 421-409 Ma (Late Silurian-Early Devonian), 358-353 m (Late Devonian-Early Carboniferous), 226-218 a (Late Triassic), and 161-144 ma (Middle-
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Age of the Siberian craton crust beneath the northern kimberlite fields: Insights to the craton evolution

TL;DR: In this article, the age distribution and trace element characteristic of zircons from kimberlites of the Kuoika field (northeastern Siberian craton), along with data compilation on the age of hosting terranes, reveal details of the evolution of the northern Siberian Craton.
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Kimberlites and megacrystic suite: Isotope-geochemical studies

TL;DR: In this paper, major and rare-earth element data on Cr-poor megacrystic suite from Yakutian kimberlites were studied in garnet, clinopyroxene, and phlogopite megacellites.