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- W2369244275 abstract "The silicified-rock-type gold deposits are hosted in silicified tuffaceous conglomerate and silicified tuff, which are part of the Acidic-Ash-Tuff Formation of the Lower Carboniferous Dahalajunshan Group.They are characterized by low grade, large reserve, near surface and strata-bound.The generalization can be divided into three metallogenic stages: primary sedimentary concentration, hydrothermal alteration and epigenetic oxidation and leaching. Fluid inclusion, although it is rare and tiny, studies show that the liquid phase is dominant with gas/liquid phase from 5% to 10% ,The ore-forming fluid is commonly meteoric water, and with minor magmatic water. The salinity is No.39wt% NaCI, pH=5.5 and Eh=-0.8-1.2 V.The metallogenic temperature(T) is 88°-98°, Pressure (P)=59×10 Pa and Depth (H)=230 m.It is concluded that the silicified-rock-type gold deposits are formed by an epithermal system." @default.
- W2369244275 created "2016-06-24" @default.
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- W2369244275 date "2000-01-01" @default.
- W2369244275 modified "2023-09-25" @default.
- W2369244275 title "THE CHARACTERISITICS AND GENESIS OF SILICIFIEDROCK -TYPE GOLD DEPOSITS IN TULASI, YINING" @default.
- W2369244275 hasPublicationYear "2000" @default.
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