联合RGB属性融合与FCM聚类算法的浅海浊积砂体精细表征以莺歌海盆地X气田为例

    Detailed characterization of shallow marine turbidite sand bodies using RGB attribute fusion and FCM clustering algorithm: a case study of X Gas Field in the Yinggehai Basin

    • 摘要: 浅海浊流沉积体系控制下X气田浊积砂体沉积特征复杂、空间展布不清,制约着油气资源的开发。基于测井、岩芯、三维地震等资料,联合分频RGB属性融合技术与FCM聚类算法开展浊积砂体精细表征,取得以下3点认识:①研究区浊积砂体表现出强振幅高连续性的地震反射特征,15、35、55 Hz分频地震属性切片的RGB融合效果与浊积砂体的空间展布响应程度最佳,砂体预测厚度与实际钻遇砂体厚度较为吻合,相关系数R2约为0.94;②FCM算法能够完成优选地震属性的有效聚类,依据5个聚类组的平面特征,初步划分出3类浊积砂体;③研究区泥质沉积背景上发育带状侧积体、环状侧积体、水道堤岸、水道-分支水道、近端朵体、远端朵体6类沉积单元,预测环状、带状侧积体、远端朵体为有利砂体。

       

      Abstract: The deposition characteristics of turbidite sand bodies in the X gas field in the Yinggehai Basin, South Chin Sea, controlled by shallow marine turbidity current sedimentary systems, are complex and spatially distributed unclearly, which restricts the development of oil and gas resources. Based on well logging, core, and 3D seismic data, we combined frequency decomposition RGB attribute fusion technology with the FCM clustering algorithm and achieved a fine characterization of turbidite sand bodies. Results show that ① The turbidite sand bodies have strong amplitude and high continuity in seismic reflection. The RGB fusion of frequency-decomposed seismic attributes at 15, 35, and 55 Hz best responded to the spatial distribution of turbidite sand bodies, and the predicted sand body thickness well matched the actual thickness seen in drill hole, showing a high correlation coefficient (R2=0.94). ② The FCM algorithm effectively clustered the selected seismic attributes, and divided the turbidite sand bodies into three main categories based on the planar features of five clustering groups. ③ In the muddy sedimentary background, six sedimentary units could be recognized, i.e., banded lateral accumulation bodies, annular lateral accumulation bodies, channel banks, channel-branch channels, proximal lobe bodies, and distal lobe bodies. The annular and banded lateral accumulation bodies, as well as the distal lobe bodies, are good targets for sand mining.

       

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