沟西铁矿区构造对水文地质条件的影响分析
The Influences Analysis on Tectonic Condition to Hydrogeologic Condition in Gouxi Iron Area

DOI: 10.12677/GSER.2015.43012, PP. 110-115

Keywords: 构造条件，水文地质条件，控制因素，沟西铁矿区
Tectonic Condition, Hydrogeologic Condition, Controlling Factors, Gouxi Iron Mine Area

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Abstract:

本文在分析了沟西铁矿区地质构造特征的基础上，查明了矿区含水层性质并探讨了构造条件对水文地质特征的控制作用。认为矿区水文地质条件为中等，褶皱及断裂构造的发育是矿区水文地质条件的主要控制因素。
Based on the analysis on tectonic condition, the paper ascertains aquifer’s property, and then ex-plores control function of Tectonic Condition on Hydrogeologic Condition in Gouxi Iron Area. It turns out that Hydrogeologic Condition is intermediate complex, and the development of folds and faults is the main controlling factor to Hydrogeologic Condition.

References

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[2]	GB 12719-91 (1991) 矿区水文地质工程地质勘探规范. 国家技术监督局, 北京.

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