沃林高原(挪威海)始新世-始新世沉积物中二基因转化的定量参数取决于其沉积条件

IF 0.3 Q4 GEOLOGY
K. V. Syromyatnikov, R. R. Gabdullin, M. A. Levitan
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引用次数: 0

摘要

摘要 通过对所研究的沃林高原钻孔剖面中的铁、锰和钙含量的分布以及海洋沉积物沿深度的密度进行一维回归分析,研究了成岩转变的强度。因此,我们估算了始新世-早更新世沉积物成岩过程的定性参数。在单因素离散分析的基础上,我们还研究了沃林高原主要岩性类型沉积物成岩过程的强度。结果表明,除了断裂以及底流和浊积岩的影响之外,始新世-早更新世成岩过程的程度还取决于以下主要因素:沉积条件、沉积物的岩性组成以及沃林高原始新世-早更新世沉积物成分中的有机碳含量。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Quantitative Parameters of Diagenetic Transformations in Eocene–Pleistocene Sediments of the Vøring Plateau (Norwegian Sea) Depending on Their Sedimentation Conditions

Quantitative Parameters of Diagenetic Transformations in Eocene–Pleistocene Sediments of the Vøring Plateau (Norwegian Sea) Depending on Their Sedimentation Conditions

Abstract

The degree of intensity of diagenetic transformations was studied using one-dimensional regressive analysis of the distribution of Fe, Mn, and Corg contents, as well as the density of marine sediments along depth in the sections of the studied boreholes drilled on the Vøring Plateau. As a result, we estimated the qualitative parameters of diagenetic processes in the Eocene–Pleistocene sediments. On the basis of one-factor dispersion analysis, we also studied the degree of intensity of diagenetic processes for the main lithological types of sediments of the Vøring Plateau. It is established that, in addition to hiatuses and the influence of bottom currents and turbidites, the degree of diagenetic transformations in the Eocene–Pleistocene depended on the following main factors: sedimentation conditions, lithological composition of sediments, and the amount of organic carbon in composition of the Eocene–Pleistocene sediments of the Vøring Plateau.

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来源期刊
CiteScore
0.60
自引率
25.00%
发文量
43
期刊介绍: Moscow University Geology Bulletin  is the journal that mainly publishes scientific articles, short reports of graduate students, and reviews. Publications made by the members of the Faculty of Geology of the Moscow State University and their collaborators are published. Publications encompass all branches of geology.
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