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首页> 外文期刊>Australian Journal of Earth Sciences >Sedimentology and seismic geomorphology of a lacustrine depositional system from the deep zone of the Gaoyou Sag, Subei Basin, eastern China
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Sedimentology and seismic geomorphology of a lacustrine depositional system from the deep zone of the Gaoyou Sag, Subei Basin, eastern China

机译:中国苏梅盆地的苏州凹陷深处湖泊沉积系统的沉积学和地震大形态

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Sandstones of the Dainan Formation in the Gaoyou Sag of the Subei Basin are important hydrocarbon reservoirs. This paper studies the sedimentary facies and sandstone dispersal patterns in the Gaoyou Sag, based on the analysis of sedimentology and seismic geomorphology. The data used in this study include lithological data, wire-line-log data and three-dimensional (3D) seismic data. The target strata are the Eocene Daiyi Member (E(2)d(1)(3), E(2)d(1)(2) and E(2)d(1)(1)) and the lower Daier Member (E(2)d(2)(5)), which belong to three third-order sequences. Five types of depositional systems were identified in the Dainan Formation based on core observation and log-facies analysis. They are, respectively, delta, fan delta, sub-lacustrine fan, nearshore subaqueous fan and lacustrine system. Stratal slices from 3D seismic volumes have been used to map the sandstone dispersal patterns and to document the evolution of the depositional systems within these third-order sequences and associated systems tracts. In the low-stand systems tract and the high-stand systems tract, sandstones of delta, fan delta and nearshore subaqueous fan were well developed and can be delineated by stratal slices showing distinct progradation towards the deep lake centre. In the transgressive systems tract, sandstones are less common. Stratal slices indicate that the depositional environments of individual third-order sequences evolved from gravel-rich or sand-rich fans to lacustrine mudstones, and finally to mixed sandstone-mudstone fans. Sandstone dispersal patterns appear to be primarily controlled by synsedimentary faults, and generally sandstone thickness decreases with distance from the synsedimentary faults. Deltas and fan deltas have different characteristics in sand-body thickness because they have different sedimentary subfacies. The proposed geomorphology and sedimentary evolution of the lacustrine depositional system may aid in the prediction of potential reservoir distribution in the Gaoyou Sag.
机译:沉船在薯条盆地的高邮凹陷中形成的砂岩是重要的碳氢化合物储层。本文基于沉积物和地震性地貌的分析,研究了高邮凹陷中的沉积相和砂岩分散模式。本研究中使用的数据包括岩性数据,线线 - 日志数据和三维(3D)地震数据。靶层是何益益成员(E(2)D(1)(3),e(2)D(1)(2)和e(2)d(1)(1))和下层成员(E(2)D(2)(5)),属于三个三阶序列。基于核心观察和对数分析,在Dainan形成中鉴定了五种类型的沉积系统。它们分别是三角洲,风扇三角洲,亚湖泊风扇,近岸亚基风扇和湖泊系统。来自3D地震体积的梯形切片已被用于映射砂岩分散模式并记录这些三阶序列和相关系统束中的沉积系统的演变。在低展台系统的道路和高架系统道中,德雷塔的砂岩,风扇三角洲和近岸亚基风扇均发育良好,可以通过显示朝向深湖中心的独特促成的层面划清。在近灾系统的道路中,砂岩不太常见。划分表明,个体三阶序列的沉积环境从砾石或富含砂砾的风扇演变为湖泊泥岩,最后到混合砂岩 - 泥岩风扇。砂岩分散模式似乎主要由Synsementary断层控制,并且通常砂岩厚度随着Synsementary断层的距离而降低。 Deltas和Fan Deltas在沙体厚度上具有不同的特点,因为它们具有不同的沉积亚缺口。湖泊沉积系统的拟议地貌和沉积演化可能有助于预测高邮凹陷中的潜在储层分布。

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