Rubatto D.Zircon trace element geochemistry:partitioning with garnet and the link between U-Pb ages and metamorphism[J].Chemical Geology,2002,184:123-138.
[6]
Vavra G,Schmid R,Gebauer D.Internal morphology,habit and U-Th-Pb microanalysis of amphibolite-to-granulite facies zircons:geochronology of the Ivrea (Southern Alps)[J].Contrib.Mineral.Petrol.,1999,134:380-404.
Wang S Q,Li X Y,Chen N S,et al.LA-ICP-MS U-Pb ages of zircon from metaleucosomes Olongbuluke microcontinent,North Qaidam,and implications on the response to the global Rodinia supercontinent assembly event in NW China[J].Journal of China University of Geosciences,2006,17 (3):238-245.
Williams I S.U-Th-Pb geochronology by ion microprobe[A].In:Mckibben M A,Shanks W C,Riddley W I,eds.In applications of microanalytical techniques to understanding mineralizing processes[C].Review of Economic Geology,1998,7:1-35.
Ludwig K.Isoplot/Ex 2.49:A Geochronological Toolkit for Microft.Excel.Berkeley Geochronology[M].Center,Berkeley,CA,USA,Special Publication No.1a.2001.
[19]
Wiedenbeck M.An example of reverse discordance during ion microprobe zircon dating:an artifact of enhanced ion yields from radiogenic labile Pb[J].Chem.Geol.,1995,125:197-218.
[20]
Romer R L.Alpha-recoil in U-Pb geochronology:effective sample size matters[J].Contrib.Mineral.Petrol.,2003,145:481-491.
[21]
Tichomoriwa M,Whitehouse M J,Nasdala L.Resorption,growth,solid state recrystallization,and annealing of granulite facies zircon-a case study from the Central Erzgebirge,Bohemian Massif[J].Lithos,2005,82:25-50.
