Dike Magmatism in the Evolution of the Transform Active Continental Margin of the Siberian Craton in the Ediacaran

A. E. Vernikovskaya; V. A. Vernikovsky; N. Yu Matushkin; P. I. Kadilnikov; D. V. Metelkin; Z. X. Li; S. A. Wilde; I. V. Romanova; E. A. Bogdanov

doi:10.1134/S1028334X19110266

Dike Magmatism in the Evolution of the Transform Active Continental Margin of the Siberian Craton in the Ediacaran

A. E. Vernikovskaya, V. A. Vernikovsky, N. Yu Matushkin, P. I. Kadilnikov, D. V. Metelkin, Z. X. Li, S. A. Wilde, I. V. Romanova, E. A. Bogdanov

Результат исследования: Научные публикации в периодических изданиях › статья › рецензирование

Аннотация

An Ediacaran complex of dike rocks has been identified for the first time in the Yenisei Ridge orogen. These igneous rocks are represented by basic, intermediate and acidic variants and formed in the conditions of the transform active continental margin at the stages of its development before and during the interruption of subduction and slab breakoff. The rocks range from dikes of a picrodolerite–olivine dolerite–dolerite–quartz diorite–leucogranite association with ages ranging 626‒623 Ma (U‒Th‒U isotope data for zircons, SHRIMP-II method, this work) up to adakite–gabbro-anorthosite magmatism at the end of the Ediacaran (Vernikovskaya et al., 2017).

Язык оригинала	английский
Страницы (с-по)	1285-1288
Число страниц	4
Журнал	Doklady Earth Sciences
Том	489
Номер выпуска	1
DOI	https://doi.org/10.1134/S1028334X19110266
Состояние	Опубликовано - 1 нояб. 2019

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10.1134/S1028334X19110266

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title = "Dike Magmatism in the Evolution of the Transform Active Continental Margin of the Siberian Craton in the Ediacaran",

abstract = "An Ediacaran complex of dike rocks has been identified for the first time in the Yenisei Ridge orogen. These igneous rocks are represented by basic, intermediate and acidic variants and formed in the conditions of the transform active continental margin at the stages of its development before and during the interruption of subduction and slab breakoff. The rocks range from dikes of a picrodolerite–olivine dolerite–dolerite–quartz diorite–leucogranite association with ages ranging 626‒623 Ma (U‒Th‒U isotope data for zircons, SHRIMP-II method, this work) up to adakite–gabbro-anorthosite magmatism at the end of the Ediacaran (Vernikovskaya et al., 2017).",

author = "Vernikovskaya, {A. E.} and Vernikovsky, {V. A.} and Matushkin, {N. Yu} and Kadilnikov, {P. I.} and Metelkin, {D. V.} and Li, {Z. X.} and Wilde, {S. A.} and Romanova, {I. V.} and Bogdanov, {E. A.}",

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Dike Magmatism in the Evolution of the Transform Active Continental Margin of the Siberian Craton in the Ediacaran. / Vernikovskaya, A. E.; Vernikovsky, V. A.; Matushkin, N. Yu и др.

В: Doklady Earth Sciences, Том 489, № 1, 01.11.2019, стр. 1285-1288.

Результат исследования: Научные публикации в периодических изданиях › статья › рецензирование

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AU - Vernikovsky, V. A.

AU - Matushkin, N. Yu

AU - Kadilnikov, P. I.

AU - Metelkin, D. V.

AU - Li, Z. X.

AU - Wilde, S. A.

AU - Romanova, I. V.

AU - Bogdanov, E. A.

PY - 2019/11/1

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