Black L P, Kamo S L, Williams I S, Foudoulis C, Claoué-long J C, Korsch R J and Davis D W. 2000. The quest for a high?quality zircon standard for microbeam Pb?U?Th geochronology. Geol Soc Aust Abstr, 59: 43.
[13]
Suzuki K, Shimizu H and Masuda A. 1996. Re?Os dating of molybdenites from ore deposits in Japan: Implication for the closure temperature of the Re?Os system for molybdenite and the cooling history of molybdenum ore deposits. Geochimica et Cosmochimica Acta, 60:3151-3159.
[14]
Ballard J R, Palin J M, Williams I S and Campbell L H. 2001. Two ages of porphyry intrusion resolved for the super?giant Chuquicamata copper deposit of northern Chile by ELA?ICP?MS and SHRIMP. Geology, 29:383-386.
[15]
Compston W and Pidgeon R T. 1986. Jack Hills, evidence of more very old detrital zircons in western Australia. Nature, 321:766-769.
[16]
Froude D O, Ireland T R, Kinny P D, Williams I S, Compston W, Williams I R and Myers I S. 1983. Ion microprobe identification of 4100~4200 Ma?old terrestrial zircons. Nature, 304:616-618.
[17]
Harris A C, Allen C M, Bryan S E, Compbell I H, Holcombe R J and Palin J M. 2004. ELA?ICP?MS U?Pb zircon geochronology of regional volcanism hosting the Bajo de la Alumbrera Cu?Au deposit: implications for porphyry?related mineralization. Mineralium Deposita, 39:46-67.
[18]
Hirata T and Nesbitt R W. 1995. U?Pb isotope geochronology of zircon: evaluation of laser probe?inductively coupled plasma mass spectrometry technique. Geochim Cosmochim Acta, 59: 2491-2500.
[19]
Horn I, Rundnick R L and McDonough W E. 2000. Precise elemental and isotope ratio determination by simultaneous solution nebulization and laser ablation ICP?MS: Application to U?Pb geochronology. Chemical Geology, 164:281-301.
[20]
Pearce N J G, Oerkins W T, Westgate J A, Gorton M P, Jackson S E, Neal C R and Chenery S P. 1997. A compilation of new and published major and trace element data for NIST SRM 610 and NIST SRM 612 glass reference materials. Geostand Newslett, 32:153-171.