东西伯利亚海西部海底沉积物岩性组成及油气异常

IF 0.7 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
A. I. Gresov, A. V. Yatsuk, K. I. Aksentov
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引用次数: 2

摘要

在岩石学和天然气地球化学研究的基础上,综合解释了现有资料,总结分析了东西伯利亚海西部陆工构造海底沉积物中烃类气体的粒度分布、水物性、有机饱和度、浓度和地球化学参数的形成和分布的主要因素。研究区北部和中部的沉积物以无灰长粒岩为代表;南部为灰长石-泥质-沙粒岩,含湿量为- 0.6 ~ 2.0%,天然含水量(以下简称湿)为- 18 ~ 43%,密度为- 1.5 ~ 2.0 g/cm3,开孔率为- 17 ~ 33%,甲烷及其同质物浓度分别为- 0.001 ~ 5.934和0.00003 ~ 0.0312 cm3/kg, HC组分分子质量为- 16.05 ~ 22.6 g/mol,“湿”、“干”和转化系数分别为- 0.2 ~ 51,1 ~ 1999和0.2 ~ 50.8%,δ13С -СН4为-82.7 ~ -38.4‰。根据气体地球化学参数值,确定了11种底部沉积物气源类型。结果表明,沉积物中HC异常的形成主要受储层物性、碳含量、采样深度以及下伏沉积物含气饱和度、气源类型、断裂和褶皱构造、构造位置、第四纪沉积物厚度、煤和气含量、褶皱基底年龄等地质因素的综合影响。HC气体异常与沉积物的岩性组成和密度参数的关系较小。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Lithological Composition and Hydrocarbon Anomalies of Bottom Sediments in the Western Part of the East Siberian Sea

Lithological Composition and Hydrocarbon Anomalies of Bottom Sediments in the Western Part of the East Siberian Sea

Based on the lithological and gas-geochemical studies and a comprehensive interpretation of the available materials, the main factors of the formation and distribution of grain size distribution, water-physical properties, organic saturation, as well as concentrations and geochemical parameters of hydrocarbon (HC) gases in seafloor sediments of geostructures in the western part of the East Siberian Sea are summarized and analyzed. It has been established that the sediments in the northern and central parts of the studied region are represented by aleurite–pelites; in the southern part, by aleurite–pelite–psammites with the following parameters: Corg—0.6–2.0%, natural moisture content (hereafter, wetness)—18–43%, density—1.5–2.0 g/cm3, open porosity—17–33%, concentrations of methane and its homologs—0.001–5.934 and 0.00003–0.0312 cm3/kg, respectively, molecular mass of the HC fraction—16.05–22.6 g/mol, coefficients of “wetness”, “dryness”, and transformation—0.2–51, 1–1999, and 0.2–50.8%, respectively, and δ13С‒СН4 varying from –82.7 to –38.4‰. Based on the values of gas-geochemical parameters, eleven types of gas sources were identified in bottom sediments. The results showed that the formation of HC anomalies in sediments is governed mainly by their reservoir properties, Corg content, sampling depths, integrated influence of geological factors, such as gas saturation of the underlying sediments, type of gas sources, fault and fold tectonics, position of geostructures, thickness of Quaternary sediments, content of coal and gas, and age of the folded basement. Anomalies of HC gases are associated to a lesser extent with the lithological composition and density parameters of sediments.

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来源期刊
Lithology and Mineral Resources
Lithology and Mineral Resources 地学-地球化学与地球物理
CiteScore
1.30
自引率
37.50%
发文量
29
审稿时长
>12 weeks
期刊介绍: Lithology and Mineral Resources is an international peer reviewed journal that publishes articles on a wide range of problems related to the formation of sedimentary rocks and ores. Special attention is given to comparison of ancient sedimentary rock and ore formation with present-day processes. The major part of the journal is devoted to comparative analysis of sedimentary processes on the continents and in oceans, as well as the genetic aspects of the formation of sedimentary and hydrothermal–sedimentary mineral resources. The journal welcomes manuscripts from all countries in the English or Russian language.
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