Qu Xiaoming;Hou Zengqian;Li Youguo Melt components derived from a subducted slab in late orogenic ore-bearing porphyries in the Gangdese copper belt,southern Tibetan (Xizang) plateau [J] 2004 doi:10.1016/j.lithos.2004.01.003
[2]
Morrison G W,Characteristics and tectonic settings of the shoshonite rock association,Lithos,1980(1).
[3]
Middlemost E A K Naming materials in the magma/igneous rocks system [J] 1994 doi:10.1016/0012-8252(94)90029-9
[4]
Maniar P D;Piccoli P M Tectonic discrimination of granitoids [J] 1989 doi:10.1130/0016-7606(1989)101<0635:TDOG>2.3.CO;2
[5]
Rollinson H R,Using geochemical data:evaluation,presentation,interpretation,Harlow:Longman Scientific & Technical Limited,1993.
[6]
Riekwood P C,Boundary lines within petrologic diagrams which use oxides of minor elements,Lithos,1989.
Wu FY. ；Sun DY. ；Li HM. ；Jahn BM. ；Wilde S.,A-type granites in northeastern China: age and geochemical constraints on their petrogenesis,Chemical geology?,2002, 187(1-2).
Sylvester Paul J,Post-collisional strongly peraluminous granites,Lithos,1998.
[17]
Sun S S;McDonough W F,Chemical and isotopic systematic basalt:implication for mantle composition and processes,Geological Society Special Publication,1989.
Cox C G;Bell J D;Pankhurst R J,The Interpretation of Igneous Rocks,London:George,Allen and Unwin,1979.
[22]
Cheng Yanbo;Mao Jingwen,Age and geochemistry of granites in Gejiu area,Yunnan province,SW China:Constrains on their petrogenesis and tectonic setting,Lithos,2010.
