Clastic facies pattern recognition is somewhat systematic.
碎屑岩相模式的识别是带有一定系统性的。
The Carboniferous sequence (including the Permian in the upper part) and its sedimentary facies pattern indicate that the rocks were formed in a large basin opening toward the south.
北淮阳地区的石炭系甚至二叠系的层序和相带分布表明，它是代表一个向南开口的大型盆地。
Hence, micro seismic facies analysis can be successfully achieved using interactive interpretation system plus fuzzy dynamic clustering and pattern recognition.
据此。本文应用模糊动态聚类和模式识别相结合的方法，在人机交互解释系统上自动实现微地震相分析。
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