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- W2350447111 abstract "Yangshu Au-Ag deposits occurre in the transitional belt of interbedded marbleof Dashiqiao F.and leptite of Gaixian F,which host rocks mainly are leptite,marble and wollastonite.Their distribution are strongly controlled by nappe structure,NE-trending shearing structure and interstratal delaminating structure.Ore-forming material are polygene,mainly hypogene volcanic spouutting fluid.Magmatic hydrothermal fluids superimposed,mixed and formed into metallogenic hydrothermal.So,for Yangshu Au-Ag deposits,metallogenic process and lithologic character are metallogenic base;ductile shearing structures are metallogenic candition;magmatic hydrothermal(silicification) is the key of metallogenesis.It is considerded that Yangshu Au-Ag deposits are of volcanic spouting-ductile shearing-magmatic hydrothermal overimposing-type deposits." @default.
- W2350447111 created "2016-06-24" @default.
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- W2350447111 date "2007-01-01" @default.
- W2350447111 modified "2023-09-23" @default.
- W2350447111 title "Geological Characteristics and Metallogenic Mechanism of Yangshu Largescale au-ag Deposits in Qingchengzi Orefeld Primary Study" @default.
- W2350447111 hasPublicationYear "2007" @default.
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