乌拉尔中部和北部东坡下石炭统火山岩土层的形成条件

IF 0.7 4区地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY

Doklady Earth Sciences Pub Date : 2024-05-02 DOI:10.1134/s1028334x24601822

G. A. Petrov, A. V. Maslov

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引用次数: 0

摘要

摘要研究了乌拉尔中部和北部东坡的下石炭统火山土著岩序。研究表明，这些岩石局限于区域性走向滑动断层带，是在张斜条件下形成的。火山岩的地球化学参数与板上和板内环境的火成岩相似，这与它们在活动大陆边缘后部形成的观点一致。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

Formation Conditions of the Lower Carboniferous Volcanoterrigenous Sequences of the Eastern Slope of the Central and Northern Urals

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Formation Conditions of the Lower Carboniferous Volcanoterrigenous Sequences of the Eastern Slope of the Central and Northern Urals

Abstract

The Lower Carboniferous volcanoterrigenous sequences of the eastern slope of the Central and Northern Urals are studied. It is shown that these rocks are confined to zones of regional strike–slip faults and formed under transtension conditions. The geochemical parameters of volcanic rocks are similar to those of igneous rocks of both suprasubduction and intraplate settings, which is in agreement with ideas about their formation in the rear of the active continental margin.

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来源期刊

Doklady Earth Sciences 地学-地球科学综合

CiteScore

1.40

自引率

22.20%

发文量

138

审稿时长

3-6 weeks

期刊介绍： Doklady Earth Sciences is a journal that publishes new research in Earth science of great significance. Initially the journal was a forum of the Russian Academy of Science and published only best contributions from Russia. Now the journal welcomes submissions from any country in the English or Russian language. Every manuscript must be recommended by Russian or foreign members of the Russian Academy of Sciences.