Pearce J A,Harris S W,Tindle A G.1984.Trace element discrimination diagrams for the tectonic interpretation of granitic rocks.Journal of Petrology,25(4):956～983.
[2]
Williams I S,Claesson S.1987.Isotope evidence for the Precambrian province and Caledonian metamorphism of high grade paragneiss from the Sere Nappes,Scandinavian Caledonides,Ⅱ.Ion micro-probe zircon U-Th-Pb.Contrib.Mineral.Petrol.,97:205～217.
Compston W,Williams I S,Kirschvink J L,et al.1992.Zircon U-Pb ages for early Cambrian time-scale.J.Geol.Sco.,149..171～184.
[6]
Defant M J,Drummond M S.1990.Derivation of some modern arc magmas by melting of young subdueted lithosphere.Nature,347:662～665.
[7]
Hofmann A W.1988.Chemical differentiation of the Earth:the relationship between mantle,continental crust,and oceanic crust.Earth and Planetary Science Letters,90:297～314.
[8]
Masuda A,Nakamura N,Tanaka T.1973.Fine structures of mutually normalized rare-earth patterns of chondrites.Geoehimica et Cosmochimica Acta,37:239～248.
