The results are basically consistent with those from CBIL.

与CBIL计算的视倾角进行对比，结果基本一致。

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In the igneous rock formation, CBIL shows fractures, vugs and weathered residual gravel clearly.

在火成岩地层中，它清晰地显示裂缝、孔洞以及风化残积的砾石。

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