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Resource potential assessment of series of strata with few drilled wells in the Huizhou Sag, the Pearl River Mouth Basin, South China Sea

机译:南海珠江口盆地惠州凹陷少量钻井系列地层资源潜力评估

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摘要

Huizhou sag is located in the depression zone in the north of the Pearl River Mouth basin. In recent years, great progress has been made in the exploration focused on the deep Paleogene, opening up new areas of exploration and necessitating the evaluation of both the hydrocarbon generation potential and the exploration potential of the Paleogene. The Enping Formation and the Wenchang Formation have become new exploration series of strata. The research utilizes paleotectonic recovery, sequence stratigraphy analysis, basic parameter prediction of hydrocarbon source rock and basin modeling, as well as other techniques. It is carried out to examine the tectonic inversion effect of the Huidong low uplift, the sedimentary facies of the Wenchang Formation, hydrocarbon source rock thickness and organic carbon content in the series of strata that have not been extensively drilled, with the calculation of both the hydrocarbon generation intensity and amount from the source rock. It is considered that: (1) after sedimentation, the Wenchang Formation suffers from tectonic inversion and severe uplift and denudation, especially the Huidong low uplift, changing the sedimentary pattern; (2) during the sedimentation of the Wenchang Formation, LF13 low-lying to Huizhou 14 low-lying is at the center of the lake basin, dominated by deep lake - semi-deep lake facies, with hydrocarbon source rock developing; (3) in total, 659.46×10~8 t of hydrocarbon is generated in Huizhou sag, with total oil and gas resources with the Wenchang Formation as source rock at about 34.3232×10~8 t; (4) comparing with the parameters and results of the previous resources assessment and considering the exploration practices in the area, it is believed that the deep part of Huizhou sag still has great exploration potential as a sag with large amount of remaining oil and gas resources in Zhu I depression.
机译:惠州凹陷位于珠江口盆地北部的洼地。近年来,在深部古近系勘探方面取得了巨大进展,开辟了新的勘探领域,并需要对烃类生潜力和古近系勘探潜力进行评估。恩平组和文昌组已成为新的地层勘探系列。该研究利用古构造恢复,层序地层分析,烃源岩和盆地建模的基本参数预测以及其他技术。研究了惠东低隆起的构造反转作用,文昌组的沉积相,未广泛钻探的一系列地层的烃源岩厚度和有机碳含量,并计算了两者的差异。烃源岩的生烃强度和数量。认为:(1)文昌组沉积后,经历了构造反转,严重隆起剥蚀,尤其是惠东低隆起,改变了沉积形态。 (2)在文昌组沉积过程中,LF13低层至惠州14低层位于湖盆中心,以深湖—半深湖相为主,发育烃源岩。 (3)惠州凹陷共生烃659.46×10〜8 t,以文昌组为烃源岩,油气资源总量约为34.3232×10〜8 t; (4)与以前的资源评估的参数和结果进行比较,并考虑该地区的勘探实践,认为惠州凹陷深部作为具有大量剩余油气资源的凹陷仍具有很大的勘探潜力。在朱我郁闷中。

著录项

  • 来源
    《Energy Exploration & Exploitation》 |2014年第2期|389-412|共24页
  • 作者单位

    School of Marine Sciences, China University of Geosciences, 29 Xueyuan Rd. Handian District, Beijing 100083, China;

    Research Institute, Shenzhen Branch Company, CNOOC Ltd., 68 Jiangnan West Rd. Haizhu District, Guangzhou 510240, China;

    School of Marine Sciences, China University of Geosciences, 29 Xueyuan Rd. Handian District, Beijing 100083, China;

    School of Marine Sciences, China University of Geosciences, 29 Xueyuan Rd. Handian District, Beijing 100083, China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Inversion structure; Sedimentary facies; Wenchang Formation; Resource potential;

    机译:反转结构;沉积相;文昌组资源潜力;

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