Compston W , Williams I S, Kirschvink J L, et al. Zircon U-Pb ages for the Early Cambrian time-scale[J]. Journal of Geological Society, London, 1992, 149:171-184.
[14]
Gradstain F M, Ogg J G, Smith A G. A geological time scale[M]. Cambridge: Cambridge University Press,2004:589.
Hart Baofu, Wang Shiguang, Jahn Born-ring, et al. Depleted-mantle source for the Uhingur River A-type granites from North Xinjiang, China:geochemistry and Nd-Sr isotopic evidence, and implication for Phanerozoic crustal growth[J]. Chemical Geology, 1997, 138: 135-159.
Horn I, Rudnick R L, Mcdonough W F. Precise elemental and isotope ratio determination by simultaneous solution nebulization and laser ablation-ICPMS: Application to U-Pb geochronology[J]. Chemical Geology, 2000,167:405-425.
[26]
Ballard J R, Palin J M, Williams I S, et al. Two ages of porphyry intrusion resolved for the super-giant Chuquicamata copper deposit of northern Chile by ELA-ICPMS and SHRIMP[]]. Geology, 2001, 9:383-386.
[27]
Kosler J, Fonneland H, Sylvester P, et al. U-Pb dating of detrital zircons for sediment provenance studies-a comparison of laser ablation ICPMS and SIMS techniques[J]. Chemical Geology, 2002, 182: 605-618.
Pidgeon R T, Nemchin A A, Hitchen G J. Internal structures of zircons from Archaean granites from the Darling Range batholith: implications for zircon stability and the interpretation of zircon U- Pb ages [J]. Contributions to Mineralogy and Petrology, 1998, 132: 288-299.
[33]
Claesson S, Vetrin V, Bayan ova T, et al. U-Pb zircon age from a Devonian carbonatite dyke, Kola peninsula, Russia: a record of geological evolution from the Archaean to the Palaeozoic[J]. Lithos, 2000,51(1/2):95-108.
