地质学
振幅
滞弹性衰减因子
偏移量(计算机科学)
垂直地震剖面
地震学
小波
大地测量学
质量(理念)
因子(编程语言)
地震波
计算机科学
光学
物理
人工智能
程序设计语言
量子力学
作者
Changjun Zhang,Tadeusz J. Ulrych
出处
期刊:Geophysics
[Society of Exploration Geophysicists]
日期:2002-09-17
卷期号:67 (5): 1542-1547
被引量:206
摘要
Estimates of the quality, Q, factor are commonly obtained from vertical seismic data or stacked surface seismic data. This paper describes a method that allows Q‐factor to be estimated directly from common midpoint (CMP) gathers. Absorption of the wavefield is dependent on three parameters: frequency, traveltime in the medium, and medium Q‐factor. Assuming that the amplitude spectrum of the seismic source signature may be modeled by that of a Ricker wavelet, we derive an analytical relation between Q‐factor and seismic data peak frequency variation both along offset and vertical time direction. The Q‐factor is estimated from CMP gathers using a layer‐stripping approach.
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