• 文献检索
  • 文档翻译
  • 深度研究
  • 学术资讯
  • Suppr Zotero 插件Zotero 插件
  • 邀请有礼
  • 套餐&价格
  • 历史记录
应用&插件
Suppr Zotero 插件Zotero 插件浏览器插件Mac 客户端Windows 客户端微信小程序
定价
高级版会员购买积分包购买API积分包
服务
文献检索文档翻译深度研究API 文档MCP 服务
关于我们
关于 Suppr公司介绍联系我们用户协议隐私条款
关注我们

Suppr 超能文献

核心技术专利:CN118964589B侵权必究
粤ICP备2023148730 号-1Suppr @ 2026

文献检索

告别复杂PubMed语法,用中文像聊天一样搜索,搜遍4000万医学文献。AI智能推荐,让科研检索更轻松。

立即免费搜索

文件翻译

保留排版,准确专业,支持PDF/Word/PPT等文件格式,支持 12+语言互译。

免费翻译文档

深度研究

AI帮你快速写综述,25分钟生成高质量综述,智能提取关键信息,辅助科研写作。

立即免费体验

Machine learning and AVO class II workflow for hydrocarbon prospectivity in the Messinian offshore Nile Delta Egypt.

作者信息

Abd-Elfattah Nadia, Dahroug Aia, El Kammar Manal, Fahmy Ramy

机构信息

Geophysics Department, Cairo University, Cairo, Egypt.

Rashpetco Company, Cairo, Egypt.

出版信息

Sci Rep. 2025 Jan 28;15(1):3566. doi: 10.1038/s41598-025-86765-7.

DOI:10.1038/s41598-025-86765-7
PMID:39875438
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11775334/
Abstract

This study presents a comprehensive workflow to detect low seismic amplitude gas fields in hydrocarbon exploration projects, focusing on the West Delta Deep Marine (WDDM) concession, offshore Egypt. The workflow integrates seismic spectral decomposition and machine learning algorithms to identify subtle anomalies, including low seismic amplitude gas sand and background amplitude water sand. Spectral decomposition helps delineate the fairway boundaries and structural features, while Amplitude Versus Offset (AVO) analysis is used to validate gas sand anomalies. The entire seismic volume is classified into facies domains using machine learning, which isolates target features from seismic background data. The study area, covering 1850 km, includes major structures such as the Rosetta fault and Nile Delta offshore anticline, with reservoirs consisting of layered sandstones and mudstones. Over 90 wells, including exploration and development wells, have been drilled in the area. Seismic amplitude data, including full and partial offset stacked, were analyzed to classify gas, water, and shale zones. The workflow's performance is demonstrated through the successful identification of the low-amplitude Swan-E Messinian anomaly, characterized as a high-risk gas prospect. Machine learning techniques, specifically neural network models, were trained to differentiate seismic features such as low-amplitude gas sand from background-amplitude water sand and shale. By iterating over multiple attributes and validating the models on blind test sets and on a blind section, which excluded a known shallow gas field, the workflow significantly improved the ability to detect potential hydrocarbon reservoirs characterized by low seismic amplitude. The results show that this integrated approach reduces exploration risk, quantifies the chance of success, and enhances decision-making in well placement and hydrocarbon exploration. This method is particularly useful for identifying low seismic amplitude anomalies, which are often challenging to detect with conventional seismic analysis. (1) This study developed a workflow to detect low seismic amplitude gas fields in near-field exploration. (2) It uses a machine learning algorithm to classify and explore low-seismic-amplitude gas sand reservoirs. (3) This approach helps estimate the likelihood of success and reduces the risk associated with hydrocarbon exploration wells.

摘要
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/c6cfd4be0f5c/41598_2025_86765_Fig18_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/400aff9df4c9/41598_2025_86765_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/99afe11c2cc1/41598_2025_86765_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/c12b4b9bc876/41598_2025_86765_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/0730d3197537/41598_2025_86765_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/632496c8c104/41598_2025_86765_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/dd2a08780fb9/41598_2025_86765_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/45d831c0422d/41598_2025_86765_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/1af8f3689346/41598_2025_86765_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/884fdae6d982/41598_2025_86765_Fig9_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/b23cb08d0eeb/41598_2025_86765_Fig10_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/d80e2068c320/41598_2025_86765_Fig11_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/aafc2c34a449/41598_2025_86765_Fig12_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/fcea0eaf9e0c/41598_2025_86765_Fig13_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/fcde600dd027/41598_2025_86765_Fig14_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/e673a9b60973/41598_2025_86765_Fig15_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/6ee69b02445a/41598_2025_86765_Fig16_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/6532cf5902c5/41598_2025_86765_Fig17a_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/c6cfd4be0f5c/41598_2025_86765_Fig18_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/400aff9df4c9/41598_2025_86765_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/99afe11c2cc1/41598_2025_86765_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/c12b4b9bc876/41598_2025_86765_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/0730d3197537/41598_2025_86765_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/632496c8c104/41598_2025_86765_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/dd2a08780fb9/41598_2025_86765_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/45d831c0422d/41598_2025_86765_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/1af8f3689346/41598_2025_86765_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/884fdae6d982/41598_2025_86765_Fig9_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/b23cb08d0eeb/41598_2025_86765_Fig10_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/d80e2068c320/41598_2025_86765_Fig11_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/aafc2c34a449/41598_2025_86765_Fig12_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/fcea0eaf9e0c/41598_2025_86765_Fig13_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/fcde600dd027/41598_2025_86765_Fig14_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/e673a9b60973/41598_2025_86765_Fig15_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/6ee69b02445a/41598_2025_86765_Fig16_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/6532cf5902c5/41598_2025_86765_Fig17a_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5de/11775334/c6cfd4be0f5c/41598_2025_86765_Fig18_HTML.jpg

相似文献

1
Machine learning and AVO class II workflow for hydrocarbon prospectivity in the Messinian offshore Nile Delta Egypt.
Sci Rep. 2025 Jan 28;15(1):3566. doi: 10.1038/s41598-025-86765-7.
2
Seismic characteristics and AVO response for non-uniform Miocene reservoirs in offshore eastern Mediterranean region, Egypt.埃及东地中海海域中新世非均匀储层的地震特征及 AVO 响应。
Sci Rep. 2023 Jun 1;13(1):8897. doi: 10.1038/s41598-023-35718-z.
3
Utilizing post-stack seismic inversion for delineation of gas-bearing sand in a pleistocene reservoir, baltim gas field, nile delta, Egypt.利用叠后地震反演技术圈定埃及尼罗河三角洲巴尔蒂姆气田更新世储层中的含气砂岩。
Sci Rep. 2024 Nov 28;14(1):29596. doi: 10.1038/s41598-024-78186-9.
4
Pre-stack seismic inversion for reservoir characterization in Pleistocene to Pliocene channels, Baltim gas field, Nile Delta, Egypt.埃及尼罗河三角洲巴尔蒂姆气田更新世至上新世河道储层特征的叠前地震反演
Sci Rep. 2025 Jan 7;15(1):1180. doi: 10.1038/s41598-024-75015-x.
5
Rock typing and reservoir characterization of the Messinian Abu Madi Formation in the onshore South Abu El Naga Gas Field, Nile Delta, Egypt.埃及尼罗河三角洲陆上南阿布埃尔纳加气田梅西尼阶阿布马迪组的岩石类型与储层特征
Sci Rep. 2025 May 7;15(1):15926. doi: 10.1038/s41598-025-97780-z.
6
High resolution 3-D seismic and sequence stratigraphy for reservoir prediction in 'Stephi' field, offshore Niger Delta, Nigeria.用于尼日利亚尼日尔三角洲近海“斯特菲”油田储层预测的高分辨率三维地震和层序地层学
Sci Rep. 2024 Sep 27;14(1):22390. doi: 10.1038/s41598-024-73285-z.
7
Seismic attributes and spectral decomposition-based inverted porosity-constrained simulations for appraisal of shallow-marine lower-Cretaceous sequences of Miano gas field, Southern Pakistan.基于地震属性和频谱分解的孔隙度约束反演模拟在巴基斯坦南部米亚诺气田浅海下白垩统层序评价中的应用
Heliyon. 2024 Feb 12;10(4):e25907. doi: 10.1016/j.heliyon.2024.e25907. eCollection 2024 Feb 29.
8
Implication of the micro- and lithofacies types on the quality of a gas-bearing deltaic reservoir in the Nile Delta, Egypt.微相和岩相类型对埃及尼罗河三角洲含气三角洲储层质量的影响。
Sci Rep. 2023 Jun 1;13(1):8873. doi: 10.1038/s41598-023-35660-0.
9
An integrated study for seismic structural interpretation and reservoir estimation of Sawan gas field, Lower Indus Basin, Pakistan.巴基斯坦印度河下游盆地萨万气田地震构造解释与储层估算综合研究
Heliyon. 2023 Apr 20;9(5):e15621. doi: 10.1016/j.heliyon.2023.e15621. eCollection 2023 May.
10
Reservoir characterization of the Abu Roash D Member through petrography and seismic interpretations in Southern Abu Gharadig Basin, Northern Western Desert, Egypt.通过岩石学和地震解释对埃及西部沙漠北部阿布加拉迪格盆地南部的阿布罗阿什D段进行储层表征。
Sci Rep. 2024 Apr 18;14(1):8966. doi: 10.1038/s41598-024-58846-6.

本文引用的文献

1
Seismic characteristics and AVO response for non-uniform Miocene reservoirs in offshore eastern Mediterranean region, Egypt.埃及东地中海海域中新世非均匀储层的地震特征及 AVO 响应。
Sci Rep. 2023 Jun 1;13(1):8897. doi: 10.1038/s41598-023-35718-z.