地震纵波横波联合勘探方法寻找近地表第四系内隐伏断裂方法研究  

Joint P-wave and S-wave seismic reflection to investigate the quatermary blind fault near surface

作　　者：李颜贵[1] 蒋正中[1] 刘子龙[1] 雍凡[1] 罗水余[1] 

机构地区：[1]中国地质科学院地球物理地球化学勘查研究所,廊坊065000

出　　处：《物探化探计算技术》2014年第6期692-699,共8页Computing Techniques For Geophysical and Geochemical Exploration

基　　金：中央级公益性科研院所基本科研业务费专项(AS2007J10;AS2011G01)

摘　　要：这里主要针对城市活断层浅层地震探测存在的一些技术问题,结合北京平原区活动断裂监测专项地质调查项目,在近地表第四系未固结沉积层中,发育许多具有相当规模的隐伏断裂,虽用纵波反射地震方法能够探测到它们的存在,但不能追踪到超浅层。结合以往的纵波资料,采用小道间距纵、横波联合勘探方法,获得了目标场地较清晰地震图像资料,并用钻井验证方法的可靠性。探讨了极浅层乐夫波等干扰波引起的假异常,需要在数据处理和解释的过程中,采取相应的技术措施消除影响,为今后类似地区活断层地震调查提供技术参考和科学依据。Shallow seismic reflection techniques have been successfully used to investigate active fault for decades.Howev-er,obtaining high-resolution seismic reflection images of ultra shallow subsurface features is still a challenge.Based on former geologic survey,high resolution seismic images were acquired by vombined P-wave and S-wave seismic reflection with small trace interval in the plain area of Beijing where hidden fault is well developed in unconsolidated sediments on quaternary strata. The results have been supported by drilling data.Furthermore,several technical methods had been applied to eliminate the effect of fake abnormalities caused by love wave in data processing and interpretation.

关 键 词：纵波 横波 隐伏断裂 可控震源 

分 类 号：P631.4[天文地球—地质矿产勘探]