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基于多次波逆时偏移的海洋垂直缆探测精度模拟

张子鑫 邢磊 杨慧良 李倩倩 张洪茂 尉佳 刘鸿

海洋地质前沿2024,Vol.40Issue(7):80-86,7.
海洋地质前沿2024,Vol.40Issue(7):80-86,7.DOI:10.16028/j.1009-2722.2023.105

基于多次波逆时偏移的海洋垂直缆探测精度模拟

Simulation study on the accuracy of ocean vertical cable detection based on multiples reverse time migration

张子鑫 1邢磊 2杨慧良 3李倩倩 1张洪茂 1尉佳 4刘鸿3

作者信息

  • 1. 海底科学与探测技术教育部重点实验室,中国海洋大学海洋地球科学学院,青岛 266100
  • 2. 海底科学与探测技术教育部重点实验室,中国海洋大学海洋地球科学学院,青岛 266100||青岛海洋科技中心海洋矿产资源评价与探测技术功能实验室,青岛 266237||海洋油气勘探国家工程研究中心,北京 100029
  • 3. 青岛海洋科技中心海洋矿产资源评价与探测技术功能实验室,青岛 266237||中国地质调查局青岛海洋地质研究所,青岛 266237
  • 4. 中国地质调查局青岛海洋地质研究所,青岛 266237
  • 折叠

摘要

Abstract

Marine vertical cable seismic survey is a new exploration technology that deploys hydrophones vertic-ally into the water.Compared with traditional streamer seismic survey,it has the advantages of high resolution and high signal-to-noise ratio.In view of the different characteristics of seismic illumination density duo to different marine vertical cable observation systems,the multiple reverse time migration imaging was used to conduct for-ward simulation and imaging process for vertical cable seismic acquisition based on acoustic wave equations for the Marmousi model,and the detection precision of vertical cable seismic exploration method was analyzed.Res-ults show that when the vertical cable was located in the center of the exploration area,the imaging of the explora-tion target layer was most beneficial.Imaging seismic data that contain free surface multiples could effectively in-crease the underground illumination range,making imaging results clearer in high and steep structural areas.This research is of great significance to the design of marine vertical cable seismic exploration observation systems and high-precision imaging process.

关键词

垂直缆/逆时偏移/多次波/正演模拟/精度分析

Key words

vertical cable/reverse time migration/multiples/forward simulation/precision analysis

分类

海洋科学

引用本文复制引用

张子鑫,邢磊,杨慧良,李倩倩,张洪茂,尉佳,刘鸿..基于多次波逆时偏移的海洋垂直缆探测精度模拟[J].海洋地质前沿,2024,40(7):80-86,7.

基金项目

中央高校基本科研业务费(202262008) (202262008)

国家重点研发计划项目(2022YFC2803503) (2022YFC2803503)

国家自然科学基金(4227655) (4227655)

中国海洋大学研究生自主科研项目 ()

海洋地质前沿

OA北大核心CSTPCD

1009-2722

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