THE VENDIAN VILYUCHAN HORIZON IN THE NYUYA ZONE IN THE SOUTH-EAST OF THE SIBERIAN PLATFORM

Q4 Earth and Planetary Sciences
N. V. Melnikov, L. V. Ryabkova
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引用次数: 0

Abstract

The present paper gives the structure analysis of the lower section part of Riphean-Vendian sediments of the Nyuya zone in the south-east of the Siberian Platform. The study results showed a complex heterochronous structure of the Talakan Formation section. The sharp difference in lithological rock composition, presence of depositional breaks of the Lower Talakan Subformation does not allow leaving this part of the section as a part of the Talakan Formation. It is proposed to refer the deposits of the lower part of the Talakan Formation to the older ones. The article is a continuation of series of works devoted to the improvement of stratigraphic schemes for the Vendian-Riphean of the Siberian Platform.
西伯利亚地台东南部尼尤亚区的维柳堪地层
本文对西伯利亚地台东南部的努亚区里皮安-文地安沉积物下段部分进行了结构分析。研究结果表明,塔拉干地层剖面具有复杂的异相结构。岩性岩石组成的巨大差异、下塔拉干亚构造沉积断裂的存在,都不允许将这部分地段作为塔拉干构造的一部分。建议将塔拉干岩层下部的沉积物归入老岩层。这篇文章是致力于改进西伯利亚地台文迪-两迭纪地层方案的系列文章的继续。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Geology and Mineral Resources of Siberia
Geology and Mineral Resources of Siberia Earth and Planetary Sciences-Geology
CiteScore
0.30
自引率
0.00%
发文量
23
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