散射波地震勘探技术在浅表层结构精细勘查中的应用研究

2013年 52卷 第No. 1期
阅读:87
查看详情
Application of seismic scattering profile technique in the shallow fine exploration
1.中国石油化工股份有限公司石油物探技术研究院,江苏南京211103;2.江苏省地质勘查技术院,江苏
南京210008
Yu Li,Sinopec Geophysical Research Institute,Nanjing 211103,China
当地震波入射到地下时,地层介质中反射波和散射波同时存在,用单一的反射理论或散射理论来描
述介质的空间结构都是不全面的。特别是结构十分复杂的浅表层介质具有强烈的不均匀性,是散射源的
主要分布区域,采用散射波地震勘探技术来研究其波场特征更具合理性与针对性。工程勘查中目前应用
的地震散射剖面法(SSP)以地震散射理论为基础,通过反射与散射的混合模型来解析地下空间结构,有利
于提高浅表层小尺度离散地质体勘查资料的信噪比和分辨能力。SSP法在隧道路线方案比选工程勘查中的
应用结果表明,在地表和地下复杂程度及震源能量基本相同的情况下,SSP资料的探测深度和信噪比均优
于常规反射地震资料;工程钻探结果印证了SSP法所获信息的可靠性。散射波地震勘探技术在工程勘查应
用中取得的研究成果,对油气地震勘探中低信噪比地区复杂近地表结构的精细地质调查具有现实的参考
意义。
When the seismic wave enters underground,reflection and scattering wave coexist in the formations.It is not
enough to describe the spatial structure by a single theory of either reflection or scattering theory.Complex shallow
media has strong heterogeneity,which is the main distribution area of scattering source.Utilizing seismic
scattering wave to study the characteristics of the wavefield is more reliable.Seismic scattering profile technique
(SSP) in engineering investigation is based on scattering theory,which utilizes the hybrid model of reflection and
scattering to resolve the structure of underground space.SSP can increase discrete shallow small scale geological
prospecting information and improve the S/N & resolution of seismic data.The application of SSP method in tunnel
sites survey revealed that the probing depth and S/N is superior to the conventional seismic reflection data.Drilling
results confirmed the reliability of SSP result.The application results provide a reference for fine geologic survey at
complex near-surface area with low S/N in hydrocarbon seismic exploration.
散射波; 浅表层结构; 地震散射剖面法; 散射成像; 异常解析;
scattering wave; shallow-surface structure; seismic scattering profile (SSP); scattering wave imaging
; anomaly interpretation
;
10.3969/j.issn.1000-1441.2013.01.007