刘希新, 于克君. 兖州西部奥陶系水文地质特征[J]. 煤田地质与勘探, 2002, 30(1): 38-40.
引用本文: 刘希新, 于克君. 兖州西部奥陶系水文地质特征[J]. 煤田地质与勘探, 2002, 30(1): 38-40.
LIU Xi-xin, YU Ke-jun. Hydrogeologic characteristics of Ordovician system in West Yanzhou, Shandong Province[J]. COAL GEOLOGY & EXPLORATION, 2002, 30(1): 38-40.
Citation: LIU Xi-xin, YU Ke-jun. Hydrogeologic characteristics of Ordovician system in West Yanzhou, Shandong Province[J]. COAL GEOLOGY & EXPLORATION, 2002, 30(1): 38-40.

兖州西部奥陶系水文地质特征

Hydrogeologic characteristics of Ordovician system in West Yanzhou, Shandong Province

  • 摘要: 华北地区奥陶系厚度大,富水性强。本文以兖州西部水源地勘探、抽水试验资料为基础,通过对奥陶系的水文地质特征的综合研究,将奥陶系含水岩组划分为7个含水层段。该方案在鲁西南的水文地质勘探中已得到了普遍应用。

     

    Abstract: In north China, the thickness of Ordovician system is larger, the water-abundance is better. Based on data of exploring authors discussed the hydrogeologic characteristics of Ordovician system in West Yanzhou. The Ordovician system carbonate can be divided into 7 water-bearing members which has been widely used in southwest of Shandong province.

     

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