Abstract：On the basis of introducing metallogenic setting of the western Qinling area,the features of inclusion and H and O isotopes of the gold deposits in this area are studied.The results show that the gold deposits in this area, occurred mainly in epimetamorphosed clastic rocks and impure carbonate of Devonian,are characterized by multi-stage mineralization.Metallogenic fluids mostly belong to Na+-Ca2+-Cl--SO42- type thermal bittern with rich CO2 and low salinity.They mainly originated from atmosphere precipitation and were influenced by magamatism and wall-rocks of ore deposits.Mineralization was carried out under condition of middle-low temperature,weak reduction,and weak acid.
王学明, 邵世才, 汪东波. 西秦岭金矿床包裹体、氢氧同位素特征及其地质意义[J]. 地质与资源, 2000, 9(1): 44-48.
WANG Xue-ming, SHAO Shi-cai, WANG Dong-bo. THE FEATURES AND GEOLOGICAL SIGNIFICANCE OF INCLUSION AND HYDROGEN AND OXYGEN ISOTOPES IN WESTERN QINLING AREA. GEOLOGY AND RESOURCES, 2000, 9(1): 44-48.
2000, Vol. 9 
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