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试解释趵突泉的成因
更新时间: 2020-07-02 00:00:00  

主要与济南的地形结构有关系。它的南面是一片山区,是山东有名的千佛山;北面是平原,济南位于山区和平原的交界线上。这里的山区是由石灰岩组成的,而平原的泥土底下也隐藏着岩浆岩。山区的石灰岩大约是在4亿年前形成的,其质地比较纯,它以大约三十度的斜度由南向北倾斜。石灰岩本身不很紧密,有空隙、裂隙和洞穴,能储存和输送地下水。地下顺着石灰岩层的倾斜,大量地流向济南。成了济南泉水的水源。在平原下的岩浆岩,它的组织很紧密。所以地下水流到这里后碰到岩浆岩的阻挡就流不过去了。岩浆岩上又覆盖着一层不透水的粘土层,地下水就不

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