摘要
塔中I号坡折带西段台内滩储层主要发育在上奥陶统良里塔格组,其地震响应以弱振幅响应为主,与东段台缘礁特有的“丘状”外部轮廓和内部发育“串珠状强反射”的地震响应特征有明显差异。台内滩弱振幅储层的优势频段为15-25Hz。优选广义S变换分频方法进行频谱分解,用20Hz分频均方根振幅实现了台内滩储层的预测,通过带通滤波处理得到的优势频段内的纯波数据进行波阻抗反演,能有效地识别出塔中西部上奥陶统良里塔格组的台内滩储层,提高了台内滩储层的识别精度,取得了较好的应用效果。
As an important substitute area,the seismic character of the intraplatform shoal reservoirs in the western area of Tazhong is weak,which is different from the strong beaded-like and moundy-shape reflection of the reef shoal reservoirs.Its responding frequency is 15-25 Hz.According to the distribution character of real seismic data,the generalized S-transform is able to adjust the variation trend of Gaussian window function with the frequency scale to the velocity control of time window width by frequency variation.Spectral decomposition with generalized S-transform is made to qualitatively predict the reservoir distribution.Then an inversion is made to the intraplatform shoal reservoirs by using pure wave data filtered by 15-25 Hz,which improves the recognization accuracy of the mud mound beach in mesa,and achieves a good application effect.
出处
《天然气地球科学》
EI
CAS
CSCD
北大核心
2014年第11期1847-1854,共8页
Natural Gas Geoscience
基金
中国石油勘探与生产公司科技项目"海相碳酸盐岩沉积环境
岩相古地理研究与有利区带优选"(编号:2009D-1905-03)资助
关键词
碳酸盐岩
塔中北部斜坡区
台内滩
广义S变换
分频反演
Carbonate
Northern slope zone of Tazhong area
Intraplatform shoal reservoirs
Generalized S-transform
Frequency division inversion