Wiedenbeck M;Alle P;Corfu F,Three natural zircon standards for U-Th-Pb, Lu-Hf, trace element and REE analyses,Geostandards Newsletter:The Journal of Geostandards and Geoanalysis,1995.
[7]
WICKHAM S M;Alberts A D;Zanvilevich A N,A stable isotope study of anorogenic magmatism in East Central Asia,Journal of Petrology,1996.
[8]
Sylvester P J,Post-collisional alkaline granites,Journal of Geology,1989.
[9]
Stacey J S;Kramers J D,Approximation of terrestrial lead isotope evolution by a two-stage model,Earth and Planetary Sciences Letters,1975.
[10]
Ludwig KR;Isoplot:,A plotting and regression program for radiogenic-isotope data. U.S,U S Geological Survey Open-File Report,1991.
[11]
Yuan Honglin;Wu Fuyuan;Gao Shan.LA-ICPMS Zircon U-Pb age and REE of Cenozoic pluton in NE China[J].科学通报,2003(14)
[12]
King P L;White A J R;Chappell B W,Characterization and origin of aluminous A-type granites from the Lachlan fold belt, Southeastern Australia,Journal of Petrology,1997.
[13]
HongDW;Wang S G;Han B F,Post-orogenic alkaline granites from China and comparisons with anorogenic alkaline granites elsewhere,Journal of Southeast Asian Earth Sciences,1996.
[14]
HeilongjiangBureauofGeology;Mineral Resources,Regional geology of Heilongjiang Province,北京:地质出版社,1993.
[15]
Andersen T,Correctionb of common lead in U-Pb analyses that do not report 204Pb,Chemical Geology,2002.
Whalen J B;Currie K L;Chaooell B W,A-type granites: geochemical charcterstics,di-scrimination and petrogensis,Contributions to Mineralogy and Petrology,1987.