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本文介绍了用数值法评价山东枣庄十里泉水资源中,如何确定和建立含水层参数与新断裂控水构造两者间的初步关系。实例说明,这种探索基本上是可行的。一、概况枣庄位于鲁南,为一近东西向构造盆地。平原区标高为50至80米,低山丘陵区标高约200至300米。区内地表水系不发育,且多为季节性河流。出露地层有前震旦系泰山群片麻岩;震旦系土门组中厚层灰岩;寒武系下部为杂色、暗紫色页岩夹灰岩,中部为张夏组鲕
This paper introduces how to determine and establish the preliminary relationship between aquifer parameters and the structure of newly fractured water control using numerical method to evaluate the water resources of Shilizhuang in Zaozhuang, Shandong Province. The example shows that this exploration is basically feasible. I. Overview Zaozhuang is located in Lunan, a nearly east-west tectonic basin. Plains elevation of 50 to 80 meters, the hilly area elevation of about 200 to 300 meters. The surface water system in the area is not well developed, and most of them are seasonal rivers. Exposed strata include the former Sinian Taishan Group Gneiss; Sinian Tumen Formation medium-thick limestone; the lower part of Cambrian is variegated and dark purple shale intercalated limestone; the middle part is Zhangxia Formation