地震相的数字化——岩相的模糊自动识别(之一)

DIGITALIZATION OF SEISMIC FACIES-The Fuzzy Auto-Recognition of Lithology: Part I

武汉地质学院物探系

本文介绍了一种新的地震地层学解释方法——岩相的模糊识别法,即通过把岩相与地震相之间的定性描述转化为定量运算,这样,可减少人为因素的影响;此外,本文作者还提出了用函数类表示各种模式的方法。

In this paper, a new technique-the fuzzy recognition of lithology for seismic-stratigraphic interpretation, was recommended. By dealing with the relationships between lithology and seismic-facies from describing them qualitatively into calculating them quantitatively, the artifi-cally imposed influence on the final results could be reduced.