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    川中地区角探1井区茅口组优质储层地震识别及预测

    Seismic identification and prediction of high-quality reservoirs in Maokou Formation, Jiaotan 1 well field, central Sichuan Basin

    • 摘要: 四川盆地中部角探1井区茅口组位于高能滩台缘带附近,受古隆起和裂陷双重作用,发育两期滩相白云岩,呈现“一隆一缘”展布格局,勘探潜力大。但是储层非均质性强、厚度变化大等特点导致其岩性圈闭与储集体的分布刻画不清,因此茅口组优质储层精准预测是勘探开发的关键环节之一。基于茅口组储层地质特征、测井响应和地震反射模式,提出 “以滩控储”的研究思路。首先从地质资料和单井特征出发,明确茅口组早、晚两期滩储层纵向分布特征;然后进行古地貌演化恢复,厘清古地貌和滩储层的耦合关系,结合成像测井资料,对比岩心孔洞发育特征,优选优质储层层段,在正演模拟基础上,建立优质储层地震识别模式;最后综合利用地震相、古地貌、地震属性和地震反演等技术,明确研究区优质滩储层纵横向发育规律。研究结果表明研究区优质储层纵向主要发育在茅二段中上部,横向发育在PS6和PY106井区的古地貌高部位,被岩性致密体所分隔,具有独立成藏的条件,总面积约为780 km2,具有巨大的勘探潜力。

       

      Abstract: The Maokou Formation in Jiaotan 1 well field, the central Sichuan Basin, is located near the high-energy beach belt at the platform margin. Owing to the combined effects of paleo-uplift and rifting, it features two phases of beach-facies dolomite with an uplift-and-margin distribution pattern, indicating great exploration potential. However, strong reservoir heterogeneity and large thickness variations impede clear characterization of lithological traps and reservoir units. Accurate prediction of high-quality Maokou reservoirs is therefore critical to exploration and development. Based on the geological characteristics, log responses, and seismic reflection features of Maokou reservoirs, this study proposes a beach-facies-controlled reservoir model. Based on geological data and single-well characteristics, this study defines the vertical distribution of the two-phase beach-facies reservoirs in the Maokou Formation. Paleo-geomorphologic reconstruction is then performed to clarify the coupling between ancient landform and beach reservoirs. Imaging log data and core-derived pore-vug characteristics are used to optimize high-quality reservoir intervals, and seismic forward modeling generates a model for high-quality reservoir identification. Finally, seismic facies, ancient landform, seismic attributes, and seismic inversion are integrated to define the vertical and lateral distribution patterns of high-quality beach reservoirs in the study area. The results show that high-quality reservoirs are mainly developed vertically in the middle and upper parts of the Mao 2 Member and laterally in the paleo-geomorphologic highs of PS6 and PY106 well fields. Separated by tight lithologic barriers and capable of forming independent hydrocarbon accumulations, they cover a total area of approximately 780 km2, indicating great exploration potential.

       

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