新疆石油地质 ›› 2024, Vol. 45 ›› Issue (2): 244-252.doi: 10.7657/XJPG20240214

• 应用技术 • 上一篇    

真地表速度建模技术在复杂山地地震资料成像中的应用

彭更新1(), 顾小弟2, 段文胜1, 公亭2, 赵锐锐1, 王勍2   

  1. 1.中国石油 塔里木油田分公司 勘探开发研究院,新疆 库尔勒 841000
    2.东方地球物理公司 研究院,河北 涿州 072750
  • 收稿日期:2023-07-29 修回日期:2023-11-03 出版日期:2024-04-01 发布日期:2024-03-26
  • 作者简介:彭更新(1966-),男,陕西渭南人,教授级高级工程师,硕士,地震解释,(Tel)0996-2172078(Email)penggx_tlm@petrochina.com.cn
  • 基金资助:
    中国石油科技重大专项(2018E-1807)

Application of True Surface Velocity Modeling Technology to Imaging of Seismic Data in Complex Mountainous Areas

PENG Gengxin1(), GU Xiaodi2, DUAN Wensheng1, GONG Ting2, ZHAO Ruirui1, WANG Qing2   

  1. 1. Research Institute of Exploration and Development, Tarim Oilfield Company, PetroChina, Korla, Xinjiang 841000, China
    2. Geophysical Research Institute, BGP, Zhuozhou, Hebei 072750, China
  • Received:2023-07-29 Revised:2023-11-03 Online:2024-04-01 Published:2024-03-26

摘要:

传统的叠前深度偏移成像技术将偏移成像和静校正问题分开处理,在复杂山地资料处理中,由于地表条件复杂、近地表横向速度变化剧烈、高速层出露等问题,基于地表一致性假设的静校正处理会引起波场畸变,导致旅行时计算误差较大,影响深度偏移成像效果。因此,提出了一种基于真地表偏移面的全深度建模与成像技术方案,从地表高程面开始速度建模,计算旅行时,将静校正问题隐含在偏移成像过程中,在复杂山地资料处理中取得了较好的应用效果。

关键词: 复杂山地, 静校正, 初至层析, 微测井, 真地表, 速度建模, 波前构建, 射线密度

Abstract:

Conventional pre-stack depth migration imaging techniques separate the migration imaging and static correction processing. In the processing of seismic data from complex mountainous areas, due to the factors such as complex surface condition, drastic lateral velocity variation near the surface, and exposure of high-velocity interval, the static correction based on the assumption of surface consistency may cause wave field distortion. This distortion leads to big errors in calculation of travel time, affecting the effects of depth migration imaging. To solve this problem, a full-depth modeling and imaging technique based on true surface migration was proposed. This technique starts with velocity modeling and travel time calculation from the surface elevation, and addresses static correction implicitly in the migration imaging process. It has been satisfactorily applied in the processing of complex mountainous data.

Key words: complex mountainous area, static correction, first-arrival tomography, microlog, true surface, velocity modeling, wavefront construction, ray density

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