在一个大规模的Anticlinorium中控制卡斯特地下水循环上的结构性地形演变
Yu Fan1, Huaisong Ji1, Ruyang Lu1
1School of Environmental Studies, China University of Geosciences, Wuhan, Hubei, China.
Ground water
|July 4, 2023
概括
地地下水系统通过构造活动和升起而发展,导致碰撞区的深地发展. 了解这种演变对于道建设和地下水资源管理至关重要.
科学领域:
- 地质地质地质地质地质地
- 水文地质学 水文地质学
- 构造学 构造学 构造学 构造学
背景情况:
- 在构造碰撞区的岩地下水系统是复杂的.
- 了解地形演化和水地化学是描述这些系统的关键.
研究的目的:
- 调查岩水层系统和岩的时间演变.
- 为了分析沿着一个大规模的反临床室的结构性地形演变.
主要方法:
- 详细的结构地形演变分析.
- 水地化学分析,水地化学分析.
- 钻孔数据的解释.
主要成果:
- 构造学压缩和升起形成了从三叠纪到新生代的地形.
- 由于地升起而导致的碳酸盐岩的暴露,开始了岩的发展.
- 间歇性的提升导致了深层的石和完整的石地下水系统的形成.
- 确定了当地,中级和区域的地地下水系统.
结论:
- 结构性地形演变直接影响地地下水系统的发展.
- 该研究为地质路线选择和地地下水利用提供了至关重要的见解.
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