莺歌海盆地北部渐新统崖城组烃源岩地球化学特征及生排烃作用

IF 4.8 2区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Yanan Wang, Zhipeng Huo, Gaowei Hu, Jianxiang Pei, Lin Wei, Lin Hu, XiaoFei Fu, Weihong Wang, Jianbo Gao, Jingshuang Luo, Jiansheng Li
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引用次数: 0

摘要

随着天然气勘探和研究的不断深入,莺歌海盆地近年来在中深层地层方面取得了显著进展和发现。由于莺歌海盆地北部勘探不足,以往的研究主要集中在中新统储层,对渐新统崖城组烃源岩研究较少。缺乏对E3y烃源岩生排烃特征和资源潜力的综合评价,阻碍了研究区进一步勘探。利用E3y的地质和地球化学资料,建立了E3y的生排烃模型。首次提出将生排烃量划分为气量和油量,包括生排气量和生排油量。研究结果表明,E3y沉积相主要为三角洲平原沼泽相和浅海相,影响了含煤烃源岩和海相泥岩的发育。含煤烃源岩厚度和面积有限。早渐新世至晚渐新世海相泥岩厚度和面积逐渐增大。烃源岩有机质含量显著,煤的总有机碳含量为19% ~ 95%,泥岩的总有机碳含量为0.12% ~ 12.6%,以ⅲ型有机质为主,镜质组反射率为2.0% ~ 5.0%,烃源岩成熟度较高。Ro值为0.8%时达到排烃阈值,生成量为677.73 × 108 t,排烃量为441.14 × 108 t。生气量为651.2 × 108 t,生油量为30.15 × 108 t,排气量为442.63 × 108 t,排油量为5.95 × 108 t。采用成因方法,估计E3y油气资源量分别为3.28 × 108 t和0.46 × 108 t。这表明莺歌海盆地北部具有良好的勘探条件。
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 Hydrocarbon Generation and Expulsion of Oligocene Yacheng Formation Source Rocks in the Northern Yinggehai Basin

As natural gas exploration and research progress, the Yinggehai Basin has achieved notable advancements and discoveries regarding middle-deep strata in recent years. Due to insufficient exploration in the Northern Yinggehai Basin, the previous studies primarily concentrated on the Miocene reservoirs with lack of research attention on the Oligocene Yacheng Formation (E3y) source rocks. A comprehensive evaluation of the E3y source rocks, encompassing hydrocarbon generation, expulsion characteristics, and resource potential, is lacking, thereby hindering further exploration in the study area. Utilizing the geological and geochemical data of E3y, the hydrocarbon generation and expulsion model was developed. For the first time, a division of hydrocarbon generation and expulsion amount into gas and oil amount is proposed, comprising generated and expelled gas amount, as well as generated and expelled oil amount. The findings suggest that the sedimentary facies of E3y primarily consisted of delta plain swamp facies and neritic facies, influencing the development of coal-bearing source rocks and marine mudstones. The coal-bearing source rocks exhibited limited thicknesses and areas. During the early to late Oligocene, there was a gradual increase in thickness and area of the marine mudstone. The source rocks exhibit a notable presence of organic matter, with total organic carbon contents ranging from 19% to 95% for coal and 0.12% to 12.6% for mudstone, predominantly composed of type III, and display high maturity indicated by vitrinite reflectance values ranging from 2.0% to 5.0%. At 0.8%, Ro reached the hydrocarbon expulsion threshold, resulting in generated and expelled amounts of 677.73 × 108 t and 441.14 × 108 t, respectively. The generated gas amount, generated oil amount, expelled gas amount and expelled oil amount are 651.2 × 108 t, 30.15 × 108 t, 442.63 × 108 t, and 5.95 × 108 t, respectively. Employing the genetic method, the gas and oil resources of E3y were estimated at 3.28 × 108 t and 0.46 × 108 t, respectively. This indicates that the Northern Yinggehai Basin presents favorable conditions for exploration.

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来源期刊
Natural Resources Research
Natural Resources Research Environmental Science-General Environmental Science
CiteScore
11.90
自引率
11.10%
发文量
151
期刊介绍: This journal publishes quantitative studies of natural (mainly but not limited to mineral) resources exploration, evaluation and exploitation, including environmental and risk-related aspects. Typical articles use geoscientific data or analyses to assess, test, or compare resource-related aspects. NRR covers a wide variety of resources including minerals, coal, hydrocarbon, geothermal, water, and vegetation. Case studies are welcome.
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