摘要
1 Introduction During the late Mesozoic times,the SE China is characterized by extensive magmatism and mineralization.The widely distributed granitoids with different(I-,S-and A-)types have been inferred to be closely related to the large-scale polymetallic mineralization.The Nanling tungsten-tin polymetallic belt is endowed with considerable
基金
Funding for the project is provided by the China Geological Survey(NO. 121201004000150015 and NO. 12120115037101)
