A groundwater level monitoring network fitting in with Jinan Karstic Spring Area has been designed.

设计出了适合济南岩溶泉域的地下水水位监测网.通过实际验证,地下水监测网符合实际要求.

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The hot groundwater occurs mainly in NE - and NW - trending faults and karstic fissure zones at their intersections.

地下热水主要赋存于 NE 与NW向断裂构造及其交汇部位的岩溶裂隙发育带中.

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