四川盆地二叠纪两类典型碳酸盐台地边缘及古地理分异格局
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1.成都理工大学;2.中国石油西南油气田公司勘探开发研究院

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国家自然科学基金区域创新发展联合基金(NO.U24A20591)、国家自然科学基金项目(编号42272132,42402120)、四川省科技计划项目(编号2023NSFSC1986)、成都理工大学优质青年人才培育特支计划(20200-000526-04)、成都理工大学珠峰科学研究计划项目(80000-2024ZF11402)和中国石油天然气股份有限公司西南油气田公司勘探开发研究院项目(No.XNS勘研院JS2022⁃2599)


Permian paleogeographic differentiation evolution and platform margin model comparison in Sichuan Basin
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1.Chengdu University of Technology;2.Petrochina Southwest Oil and Gas Field company exploration and development Research Institute

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    摘要:

    碳酸盐台地边缘是规模油气资源的重要聚集场所,明确古地理分异格局是揭示碳酸盐台地边缘性质和控滩机制的关键。继在四川盆地上二叠统长兴组台地边缘礁滩相发现万亿方天然气黄金聚集带后,最近又在中二叠统茅口组探明了台地边缘滩相储层,多口超百万方无阻气流井展现出巨大的勘探潜力。然而,这两个时期的沉积充填规律和储层类型特征具有显著差异,详细的对比分析将有助于深化碳酸盐台地模式及其控储效应的认识。本文基于四川盆地及周缘二叠系的大量钻井、野外剖面和地震资料,分析了典型的沉积相特征和岩相古地理格局,并对比了两类台地边缘的差异性。结果表明,四川盆地二叠纪古地理从茅口期开始出现多个同沉积断裂影响下的浅水台地-深水陆棚分异,形成“广元-旺苍”海槽;长兴期受拉张性构造活动影响,台地-陆棚分异进一步加剧,深水范围扩大,形成“开江-梁平”海槽。长兴组碳酸盐台地边缘发育厚层生物礁滩,茅口组碳酸盐台地边缘发育薄层云化浅滩,二者向深水区均快速转变为硅质岩和碳质泥页岩;茅口期属于初始地貌继承型台地边缘,表现为宽边缘背景下断续加积的多个薄层滩体;长兴期则为沉积镶边塑造型台地边缘,呈现出窄边缘背景下连续加积或进积的厚层礁滩体。总体上,两类台地边缘皆具有发育规模储层的潜力,可以作为大型油气聚集带勘探的重要领域。

    Abstract:

    The carbonate platform margin is an important gathering place of large-scale oil and gas resources, and the study of paleogeographic differentiation is the basis to reveal the characteristics and development laws of the carbonate platform margin. Following the discovery of a trillion square meter natural gas gold accumulation zone in the platform margin reef-beach facies of the Upper Permian Changxing Formation in Sichuan Basin, the platform margin beach reservoir of the Middle Permian Maokou Formation has recently been discovered, and several open flow wells of more than one million square meters have shown great exploration potential. However, there are significant differences in sedimentary filling and reservoir characteristics between these two periods, and detailed comparative analysis will help deepen the understanding of carbonate platform model and its reservoir control effect. Based on a large number of drilling, field outcrop and seismic data from the Sichuan Basin and its surrounding Permian system, the typical sedimentary facies and lithofacies paleogeographic pattern are analyzed, and the differences between the two types of platform margins are compared. The results show the differentiation from shallow-water platform to deep water shelf by multiple synsedimentary faults occurred in Permian paleogeography of Sichuan Basin from Maokou period, with Kaijiang-Liangping trough being the most typical. The shallow-water carbonate platform of Changxing Formation is characterized by the development of thick platform margin reef-beach facies, and the shallow-water carbonate platform of Maokou Formation is characterized by the development of thin platform margin beach facies, both of which rapidly change into siliceous rock and carbonaceous shale. The Maokou period belongs to the initial geomorphic inherited platform margin, which is represented by several thin beach bodies with intermittent accretion under the background of wide margin. In the Changxing period, the platform margin was shaped by sedimentary border, showing a thick reef flat body with continuous accretion or prograding under the background of narrow margin. In general, both platform margins have the potential to develop large-scale reservoirs and are important targets for exploration of large oil and gas accumulation zones.

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  • 收稿日期:2024-08-28
  • 最后修改日期:2024-12-05
  • 录用日期:2024-12-09
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