首页|主动源全波形反演在内蒙古居延海坳陷多资源勘查中的应用

主动源全波形反演在内蒙古居延海坳陷多资源勘查中的应用

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主动源全波形反演(Full Waveform Inversion,FWI)是一种基于波形匹配的高分辨率成像方法,近年来在近地表高分辨率成像中得到了较多的实际应用.然而,由于周期跳跃等因素导致的强非线性特征使得该方法对初始模型的准确性和地震数据的质量具有较高的依赖性.初始模型与地下实际结构较大的偏差、数据中的噪声及低频成分缺失等问题都会导致反演过程中陷入局部极小值,从而难以收敛到真实的速度结构.目前,FWI主要用于处理海上数据,在短偏移距陆地数据的应用中仍面临着较大挑战.内蒙古居延海坳陷拥有丰富的煤和油气资源,勘探开发潜力很大,但由于地质条件较为复杂,构造不清,迫切需要对地下进行高精度、高分辨率成像以进行细致研究.本研究利用该地区采集的可控震源地震勘探数据,采用多目标函数FWI获得了 2 km以浅的高精度纵波速度结构.同时,通过波形对比验证了速度模型的准确性,并基于波形反演获得的速度模型进行Kirchhoff叠前深度偏移,获得了高分辨率的深度域反射剖面.成像结果揭示了研究区域的4套主要沉积地层,为后期对该区域的进一步研究提供了重要依据,并通过程序开源共享为国内大量主动源活动构造探测提供了一套可靠的高分辨率反演成像流程.
Application of active-source full waveform inversion in multi-resource exploration in Juyanhai depression of Inner Mongolia
Full waveform inversion(FWI)is a high-resolution tomography method based on waveform matching,which has been increasingly used in practical applications in near-surface high-resolution imaging in recent years.However,due to the strong nonlinear characteristics caused by cycle skipping and other factors,FWI is highly dependent on the initial model and the quality of seismic data.Large difference between the initial model and the actual subsurface structure,the noise in the data and lack of low-frequency contents can all result in convergence into local minima in the inversion process.Currently,FWI is primarily used for processing marine data,and it still faces significant challenges when applied to short-offset land data.The Juyanhai depression region in Inner Mongolia has a large amount of coal,oil and gas resources,with substantial potentials for exploration and development.However,due to its complex geological conditions and obscure structural formations,it is urgent to carry out high-resolution subsurface imaging with great accuracy for detailed research.In this study,using controlled-source seismic exploration data from this region,we apply FWI with multiple objective functions to obtain an accurate P-wave velocity structure for depth down to 2 km.The accuracy of the velocity model is verified through waveform comparisons,and Kirchhoff pre-stack depth migration is carried out based on the velocity model obtained by waveform inversion,to obtain a high-resolution depth domain reflection profile.The imaging results nicely reveal the four main sedimentary strata in the study area,and provide crucial foundations for further research in the region.This study also offers a reliable high-resolution inversion workflow for active-source explorations in different tectonically active regions in China by sharing an open-sourced software package.

Full waveform inversionLand active source explorationPre-stack depth migrationJuyanhai depression

郑雪静、李俊伦、熊强青、解建建、李海鹏、谭静、刘增祺、段涛

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安徽省勘查技术院(安徽省地质矿产勘查局能源勘查中心),合肥 230031

中国科学技术大学地球和空间科学学院,合肥 230026

GeophysicsDepartment,Stanford University,CA,Stanford,USA

中国地震局地球物理勘探中心,郑州 450002

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全波形反演 陆地主动源勘探 叠前深度偏移成像 居延海坳陷

自然科学基金地震联合基金重点支持项目科技部重点研发项目

U21392042021YFC3000600

2024

地球物理学报
中国地球物理学会 中国科学院地质与地球物理研究所

地球物理学报

CSTPCD北大核心
影响因子:3.703
ISSN:0001-5733
年,卷(期):2024.67(8)