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- W2368403426 abstract "Summary:Shidonggou silver polymetallic deposit is located at the west Caledonian orogenic zone in north Qilian,which is belonged to the identical mineralization series with Taergou large-scale tungsten deposit.The strata in the mining area are the Pre-Changchengian Beidahe group,which is a set of middle-kata metamorphism rocks.Shidonggou fault(F1) is one of the major controlling faults in the area.It strictly controls the ore belt.The ore body resembles layered.The orebearing rock is brecciated and silicified limestone.The silver mineralization is positively related to the lead mineralization,and negatively related to the zinc mineralization.The orebody grade and thickness show the characteristics of expanding,reduction,and partition concentration.The ore body plunges to the east.The ore belt extends along the EW direction.The prospecting prospect is broad along the fault zone.The ore body boundary is not yet controlled in the deposit depth portion and along the EW extending direction.The prospecting space is large in the east mine field.The indication effect of ditch and soil anomaly is obvious.It is exceptionally open to the west.The prospecting prospect is big in the west area." @default.
- W2368403426 created "2016-06-24" @default.
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- W2368403426 date "2009-01-01" @default.
- W2368403426 modified "2023-09-23" @default.
- W2368403426 title "Analysis of ore enrichment regularity and the prospecting foreground for Shidonggou silver polymetallic deposit in Gansu Province" @default.
- W2368403426 hasPublicationYear "2009" @default.
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