岩性油气藏 ›› 2023, Vol. 35 ›› Issue (4): 6169.doi: 10.12108/yxyqc.20230406
王立德1, 王小卫1, 周辉2, 吴杰1, 张志强3, 王建乐1, 王德英1, 冯刚1
WANG Lide1, WANG Xiaowei1, ZHOU Hui2, WU Jie1, ZHANG Zhiqiang3, WANG Jianle1, WANG Deying1, FENG Gang1
摘要: 陆上地震资料由于低频信息缺失、波场复杂等问题,加剧了反演的非线性。基于改进共轭梯度法的时间域多尺度分层反演方法有效重建了纵、横波速度场。研究结果表明: ①利用时窗筛选早至波信息,使用小炮检距早至波数据自低频至高频多尺度重建浅层速度场,可以减少中深层反射波及噪声的强非线性影响;固定浅层速度,采用全波场的全偏移距数据可重建中深层速度场。②整个反演过程均利用基于移动加权平均的改进共轭梯度法进行速度场的迭代更新。改进的共轭梯度法可增强反演的稳定性,提高深层速度建模质量,同时反演收敛更快;分层反演策略可兼顾浅层低速和深层高速,采用大小不同的有限差分网格,保证波场模拟精度的同时减少了计算量,提高了反演计算效率;改进共轭梯度法的多尺度分层反演策略可有效降低陆上实际资料带来的非线性影响,使共成像点道集拉平程度更好,纵、横波速度场均得到有效恢复。
中图分类号:
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