| 和村-孙庄盆地富锶矿泉水赋存地质条件 |
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| 引用本文： | 常明华.和村-孙庄盆地富锶矿泉水赋存地质条件[J].中国煤炭地质,2008,20(2):24-26. |
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| 作者姓名： | 常明华 |
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| 作者单位： | 常明华（河北省煤田地质勘查院,河北,邢台,054000） |
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| 摘 要： | 和村-孙庄盆地锶矿泉水属低钠低矿化度含锶重碳酸钙镁型中性低温矿泉水。通过对盆地构造、岩溶发育、地下水动态等特征的分析与研究认为，奥陶系中统峰峰组二、三段岩溶裂隙含水层为盆地内的主要富锶矿泉水地层，锶元素来源于碳酸盐和岩浆岩，矿泉水中氚浓度（33．86±3．44TU）含量表明，该矿泉水形成年龄为10～20a，具有远源补给、深层循环特征。
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| 关 键 词： | 锶矿泉水 赋存特征 岩溶裂隙含水层 峰峰组二、三段 和村-孙庄盆地 |
| 文章编号： | 1674-1803(2008)02-0024-03 |
| 修稿时间： | 2007年12月13 |
Geological Hosting Condition of Strontium Contained Mineral Water in Hecun-Sunzhuang Basin |
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| Chang Minghua.Geological Hosting Condition of Strontium Contained Mineral Water in Hecun-Sunzhuang Basin[J].Coal Geology of China,2008,20(2):24-26. |
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| Authors: | Chang Minghua |
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| Institution: | Chang Minghua (Hebei Provincial Coal Geological Exploration Institute, Xingtai, Hebei 054000) |
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| Abstract: | The strontium contained mineral water in Hecun-Sunzhuang Basin belongs to low sodium, low degree of mineralization strontium contained calcium and magnesium bicarbonate type neutral low temperature mineral water. After basin structural, karstic development and groundwater regime characteristic analyses figured out the main strontium contained mineral water aquifer is Middle Ordovlcian Fengfeng Formation members Ⅱ and Ⅲ karstic fractured aquifer, the element strontium is come from carbonate and igneous rocks, the tritium concentration in the mineral water （33.86±3.44TU） indicated that the mineral water formed age is 10-20a, and provided with characteristics of long distance recharging and deep circulation. |
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| Keywords: | strontium contained mineral water hosting character karstic fractured aquifer Fengfeng Formation members Ⅱ and Ⅲ Hecun-Sunzhuang Basin |
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