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- W2360468908 abstract "Fault structure can be both recharge area and discharge area of groundwater for the formation of in-situ sandstone-type uranium deposit. In addition,some faults,like Zhahe fault in deposit No.511 block the movement of groundwater and cause differences of hydrogeological conditions between the east side and the west side of Zhahe fault. Through constructing the recharge-runoff-discharge conditions and groundwater hydrodynamic field in the east side and the west side,it is considered that Zhahe fault is one of the reasons why the size of uranium ore formation and shape of uranium orebody between the east side and the west side of Zhahe fault are different." @default.
- W2360468908 created "2016-06-24" @default.
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- W2360468908 date "2007-01-01" @default.
- W2360468908 modified "2023-09-28" @default.
- W2360468908 title "Influences of Zhahe fault on hydrogeological conditions of deposit No.511 at the southern margin of Yili Basin" @default.
- W2360468908 hasPublicationYear "2007" @default.
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