南海东部深水重力流沉积模式与砂体构型精细刻画

    Detailed characterization of deep water gravity flow sedimentation model and sandbody configuration in eastern South China Sea

    • 摘要: 南海东部深水重力流沉积蕴含丰富的油气资源,明确沉积模式和砂体构型可指导油气高效开发。以白云凹陷东北部A气田为例,基于取芯、测井和高分辨率地震资料,明确了研究区重力流沉积类型及演化模式,完成了砂体构型表征和叠置样式分析。研究表明:A气田发育滑动-滑塌、非限制性水道、溢岸、水道化朵叶4种重力流沉积微相,ZJ7段以水道化朵叶沉积为主,ZJ6段发育滑动-滑塌沉积和多期水道-溢岸沉积。单期水道厚度约为16~31 m,宽度约280~330 m,单期朵叶厚度约为16~22 m,宽度约为400~650 m。砂体叠置样式分为离散型、叠加型和切叠型,叠置方向以水平为主,其中,叠置水道和朵叶构成了优势储层。建立了沉积相控-水道朵叶嵌套的三维精细地质构型模型,为油气精细开发提供支撑。

       

      Abstract: The deep water gravity flow deposits in the eastern South China Sea contain abundant oil and gas resources. Understanding the sedimentation model and sandbody configuration can guide the efficient oil and gas development. Taking A gas field in the northeast of Baiyun Depression as an example, based on coring, logging and high-resolution seismic data, the sedimentary types and evolution models of gravity flow are defined, the sand body configuration characterization and superposition pattern analysis are completed. The research shows there are four kinds of gravity flow sedimentary microfacies in A gas field: sliding-slumping, unconfined channels, overbank and channelized lobes. ZJ7 is dominated by channelized lobe deposits, and ZJ6 is dominated by sliding-slumping deposits and multi-phase water channel-overbank deposits. The thickness of the single channel is about 16m-31m, the width is about 280 m-330 m, the thickness of the single lobe is about 16 m-22 m, the width is about 400 m-650 m. The sand body superposition patterns are classified as discrete, superimposed and cut superimposed types, and the superposition direction is mainly horizontal, in which superimposed channels and lobes constitute the dominant reservoir. A three-dimensional fine geological configuration model controlled by sedimentary facies and channel -lobe nesting was established, providing support for the fine development of oil and gas.

       

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