The research on structural development pattern and genetic mechanism provided mine construction and production with geological basis henceforth.
赵楼井田构造发育规律及成因机制的研究为今后矿井建设与生产提供了地质依据。
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。
With the same geological structural Settings, the Miocene sequence development of the Shanwang, Baojiahe, and Qingshan Basins are comparable.
在相同构造背景下，山旺盆地、包家河盆地和青山盆地的中新世对应层位的层序发育特征具有可比性。
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