CAJ | 학술논문

　　当地震波在地层中传播时，能量的衰减是介质粘弹性性质的反应。这种介质所固有的衰减特性一般用品质因子Q来描述。该文研究的是零偏VSP衰减地震波长的正演模拟，在正演算法上采用了层状介质的波长递推公式，在基于“Ganley模型”的理论下模拟出了零偏VSP合成记录。为了验证正演模拟的正确性，用质心频率偏移法（Centroid Frequency Shift，简称CFS）对理论模型的Q值进行提取。模型结果表明了该文正演方法的正确性，也证明了CFS方法的实用性。
　　당지진파재지층중전파시，능량적쇠감시개질점탄성성질적반응。저충개질소고유적쇠감특성일반용품질인자Q래묘술。해문연구적시령편VSP쇠감지진파장적정연모의，재정연산법상채용료층상개질적파장체추공식，재기우“Ganley모형”적이론하모의출료령편VSP합성기록。위료험증정연모의적정학성，용질심빈솔편이법（Centroid Frequency Shift，간칭CFS）대이론모형적Q치진행제취。모형결과표명료해문정연방법적정학성，야증명료CFS방법적실용성。
Energy attenuation is the reflection of non-elastic property of medium when seismic wave prop-agates in the straum, which attenuation characteristic of medium is usually represented by quality factor Q.This paper studies the forward modeling of zero-offset VSP attenuation seismic wave length, and the recursion formula of wave length in layered medium is adopted in the forward simulation arithmetic . Based on the Ganley model, the zero-offset synthesized VSP data is simulated .In order to verify the cor-rectness of forward modeling, the centroid frequency shift method (CFS for short) is used to inverse the Q values on the forward zero-offset VSP geological model .The model results show that the correctness of forward modeling method, which also CFS method′s practicality.