New age data on kimberlites from the Yakutian diamondiferous province

A. M. Agashev; N. P. Pokhilenko; A. V. Tolstov; V. V. Polyanichko; V. G. Mal'kovets; N. V. Sobolev

New age data on kimberlites from the Yakutian diamondiferous province

A. M. Agashev, N. P. Pokhilenko, A. V. Tolstov, V. V. Polyanichko, V. G. Mal'kovets, N. V. Sobolev

Research output: Contribution to journal › Article › peer-review

Abstract

Among the approximately 30 kimberlite fields discovered within the Siberian Craton, 25 make up the Yakutian kimberlite province. The study of the relationships between kimberlites and host rocks, fauna in xenoliths of the host rocks [1], and comparison of isotopic datings with different grades of reliability during the two decades after their discovery in 1954 has made it possible to distinguish three stages of Yakutian kimberlite magmatism: Middle Paleozoic (Late Devonian-Early Carboniferous), Triassic, and Late Mesozoic [2]. The fields of the southern part of the province formed in Middle Paleozoic, mainly in the Devonian. The northern part of the province mainly consists of Mesozoic kimberlite fields.

Original language	English
Pages (from-to)	1142-1145
Number of pages	4
Journal	Doklady Earth Sciences
Volume	399
Issue number	8
Publication status	Published - Oct 1 2004

ASJC Scopus subject areas

Earth and Planetary Sciences (miscellaneous)
Earth and Planetary Sciences(all)

Cite this

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abstract = "Among the approximately 30 kimberlite fields discovered within the Siberian Craton, 25 make up the Yakutian kimberlite province. The study of the relationships between kimberlites and host rocks, fauna in xenoliths of the host rocks [1], and comparison of isotopic datings with different grades of reliability during the two decades after their discovery in 1954 has made it possible to distinguish three stages of Yakutian kimberlite magmatism: Middle Paleozoic (Late Devonian-Early Carboniferous), Triassic, and Late Mesozoic [2]. The fields of the southern part of the province formed in Middle Paleozoic, mainly in the Devonian. The northern part of the province mainly consists of Mesozoic kimberlite fields.",

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AU - Agashev, A. M.

AU - Pokhilenko, N. P.

AU - Tolstov, A. V.

AU - Polyanichko, V. V.

AU - Mal'kovets, V. G.

AU - Sobolev, N. V.

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AB - Among the approximately 30 kimberlite fields discovered within the Siberian Craton, 25 make up the Yakutian kimberlite province. The study of the relationships between kimberlites and host rocks, fauna in xenoliths of the host rocks [1], and comparison of isotopic datings with different grades of reliability during the two decades after their discovery in 1954 has made it possible to distinguish three stages of Yakutian kimberlite magmatism: Middle Paleozoic (Late Devonian-Early Carboniferous), Triassic, and Late Mesozoic [2]. The fields of the southern part of the province formed in Middle Paleozoic, mainly in the Devonian. The northern part of the province mainly consists of Mesozoic kimberlite fields.

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New age data on kimberlites from the Yakutian diamondiferous province

Abstract

ASJC Scopus subject areas

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