Hofmann A W. 1988. Chemical differentiation of the earth: The relationship between mantle, continental, and oceanic crust. Earth and Planetary Science Letters, 90: 297?314.
[22]
Pearce J A, Harris N B W and Tindle A G. 1984. Trace element discrimination diagrams for the tectonic interpretation of granitic rocks. Journal of Petrology, 25: 956?983.
[23]
Peter D K and Roland M. 2003. Lu-Hf and Sm-Nd isotope systems in Zircon. Reviews in Mineralogy and Geoche-mistry, 53(1): 327?341.
[24]
Rapp R P, Shimizu N, Norman M D and Applegate G S. 1999. Reaction betweens lab derived melts and peridotite in the mantle wedge: Experimental constr?aints at 3.8 GPa. Chemical Geology, 160: 335?356.
[25]
Salters V T M and Hart S R. 1991. The mantle source of ocean ridges, island, arcs: The Hf-isotope connection. Earth and Planetary Science Letters, 104: 364?380.
[26]
Tafti R, Mortensen J K, Lang J R, Rebaglitim M and Oliver J L. 2009. Jurassic U-Pb and Re-Os ages for the newly discovered Xietongmen Cu-Au porphyry district, Tibet, PRC: Implications for metallogenic epochs in the southern Gangdese belt. Economic Geology, 104: 127?136.
[27]
Taylor S R and McLennan S M. 1985. The continental crust: Its composition and evolution. Oxford: Black-w?ell Scie?ntific Publication: 1?132.
[28]
Williams I S. 1998. U-Th-Pb geochronology by ion micro- probe // McKibben M A, Shanks W C and Ridley W I. Applications of Microanalytical Techniques to Under- st?a-nding Mineralizing Processes. Reviews in Economic Geology, 7: 1?35.
Atherton M P and Petford N. 1993. Generation of sodium- rich magmas from newly underplated basaltic crust. Nature, 362: 144?146.
[51]
Chu M F, Chung S L, Song B, Liu D Y, O''Reilly S Y, Pearson N J, Ji J Q and Wen D J. 2006. Zircon U-Pb and Hf isotope constraints on the Mesozoic tectonics and crustal evolution of Southern Tibet. Geology, 34(9): 745?748.
[52]
Corfu F, Hanchar J M, Hoskin P W O and Kinny P. 2003. Atlas of zircon textures.Reviews in Mineralogy and Geoch-emistry, 53: 469?500.
[53]
Corfu F and Stott G M. 1993. Age and petrogenesis of two Late Archean magmatic suites, northwestern superior province, Canada: Zircon U-Pb and Lu-Hf isotopic relation. Journal of Petrology, 34: 817?838.
[54]
Jiang Y H, Jiang S Y, Liang H F and Dai B Z. 2006. Low?degree melting of a metasomatized lithospheric mantle for the origin of Cenozoic Yulong monzogr- anite-porphyry, east Tibet: Geochemical and Sr-Nd- Pb-Hf isotopic constraints. Earth and Planetary Scie?nce Letters, 241: 617?663.
[55]
Kamei A, Owada M, Nagao T and Shiraki K. 2004. High-Mg diorites derived from sanukitic HMA magmas, Kyushu Island, Southern Japan arc: Evidence from clinopyroxene and whole rock compositions. Lithos, 75: 359?371.
[56]
Lang X H, Tang J X, Li Z J, Huang Y, Ding F, Yang H H, Xie F W, Zhang L, Wang Q and Zhou Y. 2014. U-Pb and Re-Os geochronological evidence for the Jurassic porphyry metallogenic event of the Xiongcun district in the Gangdese porphyry copper belt, southern Tibet, PRC. Journal of Asian Earth Sciences, 79: 608?622.
[57]
Miller C, Schuster R, Klotzli U, Frank W and Purtscher F. 1999. Post-collisional potassic and ultrapotassic magmatism in SW Tibet: Geochemical and Sr-Nd- Pb-O isotopic constraints for mantle source charact?eristics and petrogenesis. Journal of Petrology, 40: 1399?1424.
[58]
Perfit M R, Gust D A, Bence A E, Arculus R J and Taylor S R. 1980. Chemical characteristics of island-arc basalts: Implication for mantle sources. Chemical Geology, 30(3): 227?256.
[59]
Samuel A B and Mark D S. 2003. High-precision U-Pb zircon geochronology and the stratigraphic record. Reviews in Mineralogy and Geochemistry, 53(1): 305?326.
[60]
Shimizu N and Masuda A. 1977. Cerium in chert as on indication of marine environment of its formation. Nature, 266 (24): 346?348.
[61]
Sun S S and McDonough W F. 1989. Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and processes // Saunders A D and Norry M J. Magmatism in the Ocean Basins. Geological Society, London, Special Publications, 42: 313?345.