[18]Qiu Y M, Groves D I, McNaughton N J, Dalstra H J. SHRIMP U-Pb in zircon andlead-isotope constraints on the timing and source of an Archaean granulite-hostedlode-gold deposit at Griffin\'s Find, Yilgarn Craton, Western Australia. Chronique De LaRecherche Miniere, 1997, 529: 91~104.
[5]
[19]Stein H J, Cathles L M. A special issue on the timing and duration of hydrothermalevents (preface). Econ. Geol., 1997, 92: 763~765.
[6]
[20]Qiu Y M, Groves D I. Late Archaean collision and delamination in the SouthwestYilgarn Craton: the driving force for Archaean orogenic lode gold mineralization? Econ.Geol., 1999, 94(1): 115~122.
[15]Williams L S. Some observation on the use of zircon U-Pb geochronology in thestudy of granitic rocks. Trans. Royal Soc. Edinburgh: Earth Sci., 1992, 83: 447~369.
[19]
[16]Miao L C, Luo Z K, Guan K, Huang J Z, Wang L G, McNaughton N J, Groves D I. ZirconSensitive High Resolution Ion Microprobe (SHRIMP) study of granitoid intrusions in ZhaoyeGold Belt of Shandong Province and its implication. Science in China, Series D, 1997,40(4): 361~369.
[20]
[17]Wang L, Qiu Y M, McNaughton N J, Groves D I, Luo Z K, Huang J Z, Miao L C, Liu YK. Constraint on crustal evolution and gold metallogeny in the NW Jiaodong Peninsula,China, from SHRIMP U-Pb zircon studies of granitoids. Ore Geology Reviews, 1998, 13: 275~291.