In the geological structural changes place, such as faults or fractured strata development often beaded reflection.

在地质结构变化明显处，如断层或缝洞发育地层常为串珠状反射。

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The extensive development of the lateral accretions of continental strata leads to the horizontal variation of lithologic character and lithologic facies.

陆相地层侧向加积作用广泛发育，导致岩性、岩相横向多变。

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Development of the Holocene strata roughly is well.

全新世地层发育基本完好。

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