彭定邦. 金山岭长城矿水床的成因[J]. 工程科学学报, 1991, 13(6): 507-513. DOI: 10.13374/j.issn1001-053x.1991.06.018
引用本文: 彭定邦. 金山岭长城矿水床的成因[J]. 工程科学学报, 1991, 13(6): 507-513. DOI: 10.13374/j.issn1001-053x.1991.06.018
Peng Dingbang. The Cause of Formation of the Jinshan Mountain Great Wall Mineral Water Deposit[J]. Chinese Journal of Engineering, 1991, 13(6): 507-513. DOI: 10.13374/j.issn1001-053x.1991.06.018
Citation: Peng Dingbang. The Cause of Formation of the Jinshan Mountain Great Wall Mineral Water Deposit[J]. Chinese Journal of Engineering, 1991, 13(6): 507-513. DOI: 10.13374/j.issn1001-053x.1991.06.018

金山岭长城矿水床的成因

The Cause of Formation of the Jinshan Mountain Great Wall Mineral Water Deposit

  • 摘要: 从地质、水文地质条件、矿泉水化学成分各方面探讨了金山岭长城矿水床的成因。从矿泉水的氢氧同位素H2、O13和H3的含量,揭示了矿水床的补给水源、补给时期、补给高程和补给位置。矿泉水的主要化学成分验证了矿水床的蓄水构造和深循环条件。

     

    Abstract: The cause of formation of Jinshan mountain Great Wall mineral water deposit in various aspects, such as geological condition, hydrogeological condition, chemical composition of the mineral water was studied. The isotopes of hydrogen and oxygen (H2, O18, H3) content in the mineral water revealed the source, age, elevation and position of recharge water of the mineral water deposit. The main chemical composition of the mineral water verified the geological structure of groundwater storage and the condition of deep water cycle.

     

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