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FLUID INCLUSION AND STABLE ISOTOPE CONSTRAINTS ON ORE GENESIS OF THE LONGSHAN ANTIMONY-GOLD DEPOSIT, HUNAN PROVINCE, CHINA

机译：湖南省湖南省龙山锑金矿床矿石成因的流体包容性和稳定同位素约束

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Geological setting, characteristics of mineralization, fluid inclusions and stable isotopes data infer that the Longshan Sb-Au deposit can be categorized into orogenic type ore deposit. Oreforming fluid derived from metamorphism during orogeny. Metals were extracted by fluids from country rocks when flowing through them.

机译：地质环境，矿化特征，液体夹杂物和稳定同位素数据推断龙山SB-Au矿床可分为造口矿床矿床。 oreforming流体在orgeny期间衍生自变质。流过它们时，通过来自乡村岩石的流体提取金属。

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《Asia Current Research on Fluid Inclusion Meeting》|2014年|1 CD-ROM|共2页
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Pang B.C.; Yang D.S.; Zhang M.; Wang B.H.; Liu X.J.; Liu Y.D.;
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FLUID INCLUSION AND STABLE ISOTOPE CONSTRAINTS ON ORE GENESIS OF THE LONGSHAN ANTIMONY-GOLD DEPOSIT, HUNAN PROVINCE, CHINA

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