Synchrosqueezing Voices Through Deep Neural Networks for Horizon Interpretation

Haifa Alsalmi, Yanghua Wang
{"title":"Synchrosqueezing Voices Through Deep Neural Networks for Horizon Interpretation","authors":"Haifa Alsalmi, Yanghua Wang","doi":"10.1190/int-2023-0121.1","DOIUrl":null,"url":null,"abstract":"Horizon picking stands as a crucial element in reservoir characterisation, yet it remains a labour-intensive process. The manual interpretation of horizons across thousands of vertical seismic slices in a 3D seismic survey significantly further amplifies the time and effort invested in this task. While several automatic methods have been developed for extracting horizons in seismic images, their effectiveness can be compromised in the presence of interruptions in lateral continuity, such as faults and noise. Additionally, closely spaced horizons pose a challenge, making it even more difficult to accurately depict their exact locations. For tracking the horizon surfaces through a 3D seismic volume, it is necessary to exploit other seismic attributes extracted from the 3D seismic data. We proposed to use spectral voice components together with the original seismic amplitudes to track target horizon surfaces. We generated the time-frequency spectrum using a high-resolution method namely the synchrosqueezing wavelet transform (SWT) method, and the real part of the complex SWT spectrum is the voice component. We imported the spectral voice component and the seismic amplitude into a neural network. A framework of deep convolutional neural network (dCNN) was adopted for tracking horizon surfaces within a 3D seismic volume. We demonstrated this application on a field seismic dataset where closely spaced thin layers are within a complex faulted formation with noisy and low signal to noise ratio seismic data. The integration of amplitude and phase within the voice component attribute demonstrates its efficacy in enhancing the quality of the generated horizons, particularly when compared to using only seismic amplitude for this task. A field data example from the F3 dataset showcases the capability of our method in accurately delineating horizons across fault surfaces and in close proximity to unconformities. This surpasses the current limitations of existing horizon-picking methods.","PeriodicalId":502519,"journal":{"name":"Interpretation","volume":"60 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-05-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Interpretation","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1190/int-2023-0121.1","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

Abstract

Horizon picking stands as a crucial element in reservoir characterisation, yet it remains a labour-intensive process. The manual interpretation of horizons across thousands of vertical seismic slices in a 3D seismic survey significantly further amplifies the time and effort invested in this task. While several automatic methods have been developed for extracting horizons in seismic images, their effectiveness can be compromised in the presence of interruptions in lateral continuity, such as faults and noise. Additionally, closely spaced horizons pose a challenge, making it even more difficult to accurately depict their exact locations. For tracking the horizon surfaces through a 3D seismic volume, it is necessary to exploit other seismic attributes extracted from the 3D seismic data. We proposed to use spectral voice components together with the original seismic amplitudes to track target horizon surfaces. We generated the time-frequency spectrum using a high-resolution method namely the synchrosqueezing wavelet transform (SWT) method, and the real part of the complex SWT spectrum is the voice component. We imported the spectral voice component and the seismic amplitude into a neural network. A framework of deep convolutional neural network (dCNN) was adopted for tracking horizon surfaces within a 3D seismic volume. We demonstrated this application on a field seismic dataset where closely spaced thin layers are within a complex faulted formation with noisy and low signal to noise ratio seismic data. The integration of amplitude and phase within the voice component attribute demonstrates its efficacy in enhancing the quality of the generated horizons, particularly when compared to using only seismic amplitude for this task. A field data example from the F3 dataset showcases the capability of our method in accurately delineating horizons across fault surfaces and in close proximity to unconformities. This surpasses the current limitations of existing horizon-picking methods.
通过深度神经网络同步声音,实现地平线解读
地层选择是储层特征描述的关键因素,但它仍然是一个劳动密集型过程。在三维地震勘探中,对数千个垂直地震切片上的地层进行人工解释,大大增加了这项工作所需的时间和精力。虽然已经开发了几种自动方法来提取地震图像中的地层,但如果横向连续性出现中断,如断层和噪声,这些方法的有效性就会大打折扣。此外,间隔较近的地平线也是一个挑战,使得准确描述其确切位置变得更加困难。要通过三维地震剖面跟踪地平线表面,就必须利用从三维地震数据中提取的其他地震属性。我们建议使用频谱声音成分和原始地震振幅来跟踪目标地平线面。我们使用高分辨率方法,即同步小波变换(SWT)方法生成时频频谱,复 SWT 频谱的实部即为语音分量。我们将频谱语音分量和地震振幅导入神经网络。我们采用了深度卷积神经网络(dCNN)框架来跟踪三维地震体中的地平线面。我们在一个野外地震数据集上演示了这一应用,该数据集中的薄层间距很近,位于一个复杂的断层地层中,且地震数据噪声大、信噪比低。将振幅和相位整合到声波分量属性中,证明了其在提高生成地层质量方面的功效,尤其是与仅使用地震振幅相比。来自 F3 数据集的一个野外数据示例展示了我们的方法在跨越断层面和接近非地层时精确划分地层的能力。这超越了现有地层选取方法的局限性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信