秋舍夫斯卡亚海洋古盆地(堪察加半岛东部):组成和发育特征

IF 1.3 4区 地球科学 Q4 OCEANOGRAPHY
N. V. Tsukanov
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引用次数: 0

摘要

摘要 本研究探讨了东堪察加秋舍夫斯卡娅盆地地层结构和组成的具体特点,该盆地形成于维特洛夫斯基盆地所在地,具有边缘海洋的性质。这一构造可能是在晚始新世-更新世开始形成的。本文提出了该构造的演变方案。在现代结构中,秋舍夫斯卡娅盆地的沉积物覆盖在各种地层的物质复合体和结构之上,并参与了该地区的增生结构。沉积地层主要是面状多变的沿海海相和/或三角洲粗沉积物,上段变为深水蜓状地层。含油现象与这些复合地层有关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Tyushevskaya Marine Paleobasin (Eastern Kamchatka): Composition and Development Features

Tyushevskaya Marine Paleobasin (Eastern Kamchatka): Composition and Development Features

Abstract

The study examines the specific features of the structure and composition of strata of the Tyushevskaya basin of Eastern Kamchatka, which formed at the site of the Vetlovsky basin, which is marginal marine in nature. This structure probably began to form in the Late Eocene–Oligocene. A scheme for its evolution is proposed. In the modern structure, sediments of the Tyushevskaya basin overlie the material complexes and structures of various terranes and participate in the accretionary structure of the region. Sedimentary formations are predominantly facies-variable coarse coastal-marine and/or deltaic sediments, which change upsection to deeper-water flysch formations. Oil-bearing manifestations are associated with these complexes.

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来源期刊
Oceanology
Oceanology 地学-海洋学
CiteScore
2.00
自引率
20.00%
发文量
83
审稿时长
6-12 weeks
期刊介绍: Oceanology, founded in 1961, is the leading journal in all areas of the marine sciences. It publishes original papers in all fields of theoretical and experimental research in physical, chemical, biological, geological, and technical oceanology. The journal also offers reviews and information about conferences, symposia, cruises, and other events of interest to the oceanographic community.
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