Cooke D R and Peter H. 2005. Giant porphyry deposits: Characteristics, distribution, and tectonic controls[J]. Econ. Geol., 100:801-817.
[7]
Defant M J and Drummond M S. 1990. Derivartion of some modern arc magmas by melting of young subduction lithosphere[J]. Nature, 662-665.
[8]
Liu Y S, Hu Z C, Gao S, Günther D, Xu J, Gao C G and Chen H H. 2008. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard[J]. Chemical Geology, 257:34-43.
[9]
Liu Y S, Gao S, Hu Z C, Gao C G, Zong K Q and Wang D B. 2010a. Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans-North China Orogen: U-Pb dating, Hf isotopes and trace elements in zircons of mantle xenoliths[J]. Journal of Petrology, 51: 537-571.
[10]
Liu Y S, Hu Z C, Zong K Q, Gao C G, Gao S, Xu J and Chen H H. 2010b. Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS[J]. Chinese Science Bulletin, 55(15): 1535-1546.
[11]
Richard H S. 2010. Porphyry copper systems [J]. Econ. Geol., 105:3-41.
[12]
更多...
[13]
Williams I S and Claesson S. 1987. Isotope evidence for the Precambrian province and Caledonian metamorphism of high grade paragneisso. from the Seve Nappes, Scandinavian Caledonides, Ⅱ. Ion microprobe zircon U-Th-Pb[J]. Contrib. Mineral. Petrol., 97: 205-217.
