The geologic discontinuous character can be recognized in coherence slices. We also can use it to study the sedimentary facies through the coherence levels.

在相干体切片上除了能够识别出地质上的不连续特征外，还可以根据相干性的级别进行目标区的沉积相研究。

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The geologic discontinuous character can be recognized in coherence slices. We also can use it to study the sedimentary facies through the coherence levels.

在相干体切片上除了能够识别出地质上的不连续特征外，还可以根据相干性的级别进行目标区的沉积相研究。

youdao