摘要
针对中国陆相沉积油层大多为薄互层的特点,根据薄互层的调谐效应物理特征,提出了采用正弦波拟合算法估计地震道频率的方法.理论模型算例和实际资料分析证明该方法对横向追踪和纵向识别薄互层是有效的.与复地震道相位求导、短时傅里叶变换、Cohen类方法相比,正弦波拟合算法估计局部数据频率具有良好的抗噪能力和分辨率.
Considering that majority of the Chinese continental reservoirs are thin inter-breeds, and based on the physical character of syntony effect of thick inter-breeds, the SinFit method is adopted to estimate the frequency of seismic trace. The method can to give more accurate and robust frequency estimates than three other common methods as phase derivative of complex trace, short time Fourier transform and Cohen class on a set of test traces where the true frequency components are known, and shows the good antinoise and high resolution. In processing the practical seismic data, the method is effectively proved to show the reservoir bed in horizontal direction and the thin inter-breeds in vertical direction.
出处
《陕西师范大学学报(自然科学版)》
CAS
CSCD
北大核心
2005年第4期40-43,共4页
Journal of Shaanxi Normal University:Natural Science Edition
基金
国家自然科学基金资助项目(40174032)
陕西省自然科学基金资助项目(2004A07)