渤海湾盆地秦南凹陷古近系烃源岩地球化学特征及油源对比

IF 4.6 3区 化学 Q2 CHEMISTRY, MULTIDISCIPLINARY
RSC Advances Pub Date : 2025-06-25 DOI:10.1039/D5RA01740H
Xukai Shi and Xiaomin Xie
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引用次数: 0

摘要

古近系沙河街组沙一段、沙三段和东营组三段是渤海湾盆地秦南凹陷重要的烃源岩。为了揭示凹陷的油气来源,详细分析了烃源岩和油的基本地球化学特征、分子地球化学特征、有机岩石学特征和正构烷烃单体碳同位素特征。结合地质环境,评价了三套烃源岩在秦南凹陷的贡献率。烃源岩总有机碳(TOC)在1.0% ~ 3.0%之间,S2-TOC表明烃源岩的质量遵循Es3 >的顺序;Es1祝辞Ed3。(2) Ed3烃源岩有机质(OM)为II2型,Es1和Es3烃源岩有机质(OM)为II1型。分子地球化学参数(CPI、C24TeT/C26TT、C27-C29正甾烷、4-MSI)表明烃源岩有机质主要来源于藻类和陆生高等植物的混合。(3) Ed3、Es1和Es3的% Ro值分别为0.61%、0.80%和0.88%。这些结果与成熟度分子参数(T-max、Ts/Tm、C29-ααα20S/(20S + 20R)和C29-ββ/(ββ + αα))一致。(4) Pr/Ph、Pr/nC17和Ph/nC18值表明三套烃源岩沉积于不同盐度的还原湖相环境(G/C30H分析),Ed3和Es3的盐度为淡水半咸水环境,而Es1的盐度为半咸水环境。(5)结合地质背景和油源对比的地球化学结果,发现沙1烃源岩对凹陷的贡献占主导地位(50%)。总体而言,本研究提供了更为准确的油源形成资料,对渤海湾盆地祁南凹陷油气勘探具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Geochemical characteristics and oil–source rock correlation in the Paleogene source rocks of the Qinnan Sag, Bohai Bay basin

Geochemical characteristics and oil–source rock correlation in the Paleogene source rocks of the Qinnan Sag, Bohai Bay basin

The Paleogene Shahejie Formation, including the first (Es1) and third (Es3) members of the Shahejie Formation, and the third member of Dongying Formation (Ed3) are important source rocks in the Qinnan Sag, Bohai Bay Basin. In order to uncover the source of oil and gas in this sag, basic geochemical, molecular geochemical, organic petrological, and n-alkane monomer carbon isotopic characteristics of source rocks and oils were analyzed in detail. In combination with the geological settings, the percentage contribution of these three sets of source rocks was assessed in the Qinnan Sag. Results obtained from the source rocks offered the following insights: (1) total organic carbon (TOC) ranged from 1.0% to 3.0%, and the S2-TOC indicated that the qualities of source rocks followed the order of Es3 > Es1 > Ed3. (2) Organic matter (OM) of the Ed3 source rock belonged to Type II2, while those of Es1 and Es3 belonged to Type II1. The molecular geochemical parameters (CPI, C24TeT/C26TT, C27–C29 regular steranes, and 4-MSI) also revealed that the organic matter in the source rocks mainly originated from mixtures of algae and terrestrial higher plants. (3) The % Ro values of Ed3, Es1, and Es3 were 0.61%, 0.80%, and 0.88%, respectively. These results were consistent with the maturity molecular parameters (including T-max, Ts/Tm, C29-ααα20S/(20S + 20R) and C29-ββ/(ββ + αα)). (4) Pr/Ph, Pr/nC17, and Ph/nC18 values indicated that the three sets of source rocks were deposited in a reduced lacustrine environment with different salinities (analyzed with G/C30H), and the salinities of Ed3 and Es3 indicated a freshwater brackish water environment, while that of Es1 suggested a brackish semi-saline water environment. (5) combining the geological settings with the geochemical results of oil–source correlations, it was found that the contribution of Es1 source rock dominated (>50%) in the sag. Overall, this study provides more accurate data of oil source formation and is significant for oil exploration in the Qinan Sag, Bohai Bay Basin.

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来源期刊
RSC Advances
RSC Advances chemical sciences-
CiteScore
7.50
自引率
2.60%
发文量
3116
审稿时长
1.6 months
期刊介绍: An international, peer-reviewed journal covering all of the chemical sciences, including multidisciplinary and emerging areas. RSC Advances is a gold open access journal allowing researchers free access to research articles, and offering an affordable open access publishing option for authors around the world.
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