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渤海湾盆地冀中坳陷饶阳凹陷肃宁地区近岸扇三角洲地震沉积学响应特征

Seismic sedimentology response characteristics of nearshore terminal fan in the suning area of Raoyang Sag, Bohai Bay Basin, NE China.

作者信息

Li Xinshuai, Meng Qingchun, Xie Jun, Wang Xiuwei, Chen Hong, Shao Minmin, Zhao Yuzhi

机构信息

College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao, 266590, China.

PetroChina Huabei Oilfield, Renqiu, 062500, China.

出版信息

Heliyon. 2024 Feb 27;10(5):e26584. doi: 10.1016/j.heliyon.2024.e26584. eCollection 2024 Mar 15.

Abstract

A nearshore terminal fan is a special water system formed in arid environments. The characterisation of its thin-channel sand bodies has long been a challenge restricting oil and gas exploration. This study takes the Suning area of the Raoyang Sag as an example and uses the principles of seismic sedimentology to conduct seismic sedimentary research on the nearshore terminal fan of the first member of the Palaeogene Shahejie Formation (Es1) based on three-dimensional seismic, logging, and core analysis. Seven fourth-order sequences (SQV7) were identified within Es1, deposited by a fluvial river system terminating at the contracting bank of a lake. Prograding terminal fan sedimentary facies on a gentle slope zone were observed in the root mean square seismic attributes after spectral decomposition. We have successfully resolved the sandstone within the studied terminal fan system using a 90° phase conversion of the seismic data and red-green-blue (RGB) fusion of the various seismic attributes. The upper subsegment of the Shahejie Formation developed extensive nearshore terminal fan sedimentation, and the seismic sedimentological response characteristics were mainly channel-like and strip-shaped geomorphic systems deposited on gentle slope zones, indicating distributary channels and distal basin sedimentation. This study enriches our understanding of nearshore fans and provides ideas for predicting favourable sand bodies in this type of sedimentary facies.

摘要

近岸末端扇是干旱环境下形成的一种特殊水动力体系。其薄河道砂体表征长期以来是制约油气勘探的难题。本研究以饶阳凹陷肃宁地区为例,基于三维地震、测井及岩心分析,运用地震沉积学原理对古近系沙河街组一段(Es1)近岸末端扇开展地震沉积研究。在Es1内识别出7个四级层序(SQV7),由一条终止于湖盆收缩岸的河流体系沉积而成。频谱分解后的均方根地震属性显示了缓坡带的进积末端扇沉积相。利用地震数据90°相位转换及多种地震属性红-绿-蓝(RGB)融合,成功分辨出研究区末端扇体系内的砂岩。沙河街组上段发育广泛的近岸末端扇沉积,地震沉积学响应特征主要为缓坡带上的似河道和条带状地貌体系,指示分流河道和远岸盆地沉积。本研究丰富了对近岸扇的认识,为该类沉积相有利砂体预测提供了思路。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1bd5/10920177/31c54ae0737b/gr1.jpg

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