Song B, Nutman A P, Liu D Y, et al. 3800 to 2500 Ma crust in the Anshan area of Liaoning Province, northeastern China[J]. Precambrian Research, 1996, 78: 79-94.
[7]
Compston W, Kinny P D, williams I S, et al. The age and lead loss behaviour of zircons from the Isua supracrustal belt as determined by ion microprobe[J]. Earth and Planetary Science letters, 1986, 80: 71-81.
[8]
Williams I S. U-Th-Pb geochronology by ion microprobe[J]. Reviews in Economic Geology, 1998, 7: 1-35.
[9]
Black L P, Kamo S L, Allen C M, et al. TEMORA 1: a new zircon standard for Phanerozoic U-Pb geochronology[J]. Chemical Geology, 2003, 200: 155-170.
[10]
Steiger R H, Jaeger E. Subcommssion on geochronology: convention on the use of decay constants in geo- and cosmochronology[J]. Earth and Planetary Science Letters, 1977, 36: 359-362.
[11]
Ludwig K R. Squid 1.02: A User\\'s Manual[M]. Berkeley Geochronology Centre: Special Publish, 2001:19.
[12]
Wan Y S, Zhang Z Q, Wu J S, et al. Geochemical and Nd isotopic characteristics of some rocks from the Paleoarchaean Chentaigou supracrustal, Anshan area, NE China[J]. Continental Dynamics, 1997, 2(1): 39-46.