摘要
Objective Sulfide inclusions within natural mineral phases play important roles in exploring the origin of magmatic sulfides ores,tracing the distribution of sulfur in mantle or crust and understanding continental mantle evolution（partial melting and metasomatism in upper mantle）.Until now,varieties of sulfide inclusions have been extensively discovered in the ultramafic or mafic phenocrysts.
Objective Sulfide inclusions within natural mineral phases play important roles in exploring the origin of magmatic sulfides ores,tracing the distribution of sulfur in mantle or crust and understanding continental mantle evolution（partial melting and metasomatism in upper mantle）.Until now,varieties of sulfide inclusions have been extensively discovered in the ultramafic or mafic phenocrysts.
基金
financially supported by the National Natural Science Foundation of China(grant No. 41302062)
the China Geological Survey(grant No. 12120115034401)
