李定龙, 周治安. 临涣矿区底含水化学特征及其形成作用探讨[J]. 煤田地质与勘探, 1994, 22(4): 37-41.
引用本文: 李定龙, 周治安. 临涣矿区底含水化学特征及其形成作用探讨[J]. 煤田地质与勘探, 1994, 22(4): 37-41.
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LI Ding-long, ZHOU Zhi-an. HYDROCHEMICAL CHARACTERISTICS OF THE FLOOR AQUIFER IN LINHUAN MINING AREA AND THEIR ORIGIN[J]. COAL GEOLOGY & EXPLORATION, 1994, 22(4): 37-41.
Citation: LI Ding-long, ZHOU Zhi-an. HYDROCHEMICAL CHARACTERISTICS OF THE FLOOR AQUIFER IN LINHUAN MINING AREA AND THEIR ORIGIN[J]. COAL GEOLOGY & EXPLORATION, 1994, 22(4): 37-41.
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临涣矿区底含水化学特征及其形成作用探讨

HYDROCHEMICAL CHARACTERISTICS OF THE FLOOR AQUIFER IN LINHUAN MINING AREA AND THEIR ORIGIN

    摘要
  • 摘要: 阐述了临涣矿区开采前、后新生界底部含水层的水化学特征及其形成作用;提出了底含水化学成因模式。对矿井底含突水水源的准确判断及井筒破裂原因分析具有积极意义。

     

    Abstract: The hydrochemical characteristics of the floor aquifer of KeinozQic before and after development in Linhuan mining area and their origin are described in detail. The hydrochemical forming model is presented. These are important for the forecast of water-inrush of the floor aquifer and the analysis of shaft fracturing.

     

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