Vol.36,No.2,2017

Other Issues:  
  

前言

前言[Abstract][PDF]

研究论文

Fracture structural analysis of Nongtun Pb-Zn deposit in Xidamingshan, Guangxi[Abstract][PDF]

Sources of ore-forming fluids and materials of Dawujian tungsten deposit in Ningguo, Anhui Province: Constraints from hydrogen-oxygen-sulfur isotope geochemistry[Abstract][PDF]

LA-ICP-MS zircon U-Pb and molybdenite Re-Os dating of Xincun Mo ore deposit in Hainan Province and its geological significance[Abstract][PDF]

Geological and geochemical characteristics and metallogenic age of Huangnikeng gold deposit in western Guangdong Province[Abstract][PDF]

Ore genesis of Tangbian Pb-Zn deposit in Tongren, Guizhou: Evidence from ore-forming fluids and isotopes[Abstract][PDF]

Fluid inclusion study and metallogenic mechanism of Xiejiagou gold deposit in Shandong Province[Abstract][PDF]

Formation age and tectonic significance of Guandi iron deposit in Yanbian area, Jilin Province[Abstract][PDF]

Metal source of Jinding superlarge lead-zinc deposit: Constraint from lead isotopic composition[Abstract][PDF]

Mineralization resulting from multistage fluids mixing at Paomaping Zn-Pb depo sit in Jinding,Lanping Basin,northwestern Yunnan Province:Evidence from ore micro-textures[Abstract][PDF]

Zoning and genesis of garnets in the Seleteguole reduced porphyry-skarn deposit of West Tianshan Mountains, Xinjiang[Abstract][PDF]

Petrogenesis of mineralized granite porphyry in Dongebi Mo deposit, Jueluotage area, Xinjiang[Abstract][PDF]

Zircon U-Pb and whole rock Rb-Sr dating of Yuanbaoshan gold deposit in Xinjiang and its geological significance[Abstract][PDF]

Magmatism and mineralization during Early Mesozoic continental accretion process in Qimantag, East Kunlun Mountains[Abstract][PDF]

Characteristics and sources of ore-forming fluid from Weixi ore block of Weibao skarn Cu-Pb-Zn deposit, Xinjiang[Abstract][PDF]

Typomorphic characteristics and genetic significance of pyrrhotite in Jinchuan Cu-Ni sulfide deposit[Abstract][PDF]

叙谈矿产地质工作

矿产资源评价篇(2)[Abstract][PDF]

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