地震走时反射层析成像研究的一些结果

Thế Hoàng Hà Phạm, Huy Hiên Đoàn, Q. Ta, Thị Lụa Mai, Hoang Anh Tu Nguyen
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引用次数: 0

摘要

速度模型在地震资料的偏移过程和时深转换中起着重要的作用,是地震资料处理的基础。有几种技术可以达到这一目标,其中层析反演是一种有效的技术。层析成像技术作为精挑细选速度分析的升级版,基于反射射线追迹和共轭梯度法估算最佳速度模型,为其他密集成像和建模模块(如逆时偏移(RTM)和全波形反演(FWI))创建初始高质量模型。鉴于上述优点,我们开发了地震走时反射层析成像(SeisT)模块,以研究该方法的准确性,同时建立地震处理的技术能力。用合成地震资料和实际地震资料对模型的精度进行了验证;开发方法和现场数据应用证明了该模型的有效性和准确性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Some results of seismic travel-time reflection tomography study
Velocity model is essential for seismic data processing as it plays an important role in migration processes as well as time depth conversion. There are several techniques to reach that goal, among which tomographic inversion is an efficient one. As an upgrade version of handpicked velocity analysis, the tomography technique is based on the reflection ray tracing and conjugate gradient method to estimate an optimum velocity model and can create an initial high quality model for other intensive imaging and modelling module such as reverse-time migration (RTM) and full-waveform inversion (FWI). For the mentioned benefit, we develop a seismic travel-time reflection tomography (SeisT) module to study the accuracy of the approach along with building the technical capability in seismic processing. The accuracy of the module has been tested by both synthetic and real seismic field data; the efficiency and the accuracy of the model have been proven in terms of development method as well as field data application.
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