Andersen T. 2002. Correction of common lead in U-Pb analyses that do not report 204Pb. Chemical Geology, 192(1？2): 59？79.
[21]
Belousova E A, Griffin W L, O’Reilly S Y and Fisher N I. 2002. Igneous zircon: Trace element composition as an indicator of source rock type. Contributions to Mineralogy and Petrology, 143(5): 602？622. B
[22]
Mushkin A, Navon O, Halicz L, Hartmann G and Stein M. 2003. The petrogenesis of A-type magmas from the Amram Massif, southern Israel. Journal of Petrology, 44: 815？832.
[23]
Nedelec A, Stephens W E and Fallick A E. 1995. The Panafrican stratoid granites of Madagascar: Alkaline magmatism in a post-collisional extensional setting. Journal of Petrology, 36: 1367？1391.
[24]
Pati?o Douce A E. 1997. Generation of metaluminous A-type granites by low-pressure melting of calc- alkaline granitoids. Geology, 25: 743？746.
[25]
Pearce J A. 1996. Sources and settings of granitic rock. Episodes, 19(4): 120？125.
Auwera J V, Bogaerts M, Liégeois J P, Demaiffe D, Wilmart E, Bolle O and Duchesne J C. 2003. Derivation of the 1.0~0.9 Ga ferro- potassic A-type granitoids of southern Norway by extreme differentiation from basic magmas. Precambrian Research, 124: 107？148.
[36]
Batchelor R A and Bowden P. 1985. Petrogenetic interpretation of granitoid rock series using multi-cationic parameters. Chemical Geology, 48(1？4): 43？55.
[37]
onin B. 1990. From orogenic to anorogenic settings: Evolution of granitoid suites after a major orogenesis. Geological Journal, 25: 261？ 270.
[38]
Boynton W V. 1984. Geochemistry of the Rare Earth Elements: Meteorite studies // Henderson P. Rare Earth Element Geochemistry. Amsterdam: Elsevier Science Publishers: 63？114.
[39]
Clemens J D, Holloway J R and White A J R. 1986. Origin of an A-type granite: Experimental constrains. American Mineralogist, 71: 317？324.
[40]
Collins W J, Beams S D, White A J R and Chappell B W. 1982. Nature and origin of A-type granites with particular reference to Southeastern Australia. Contributions to Mineralogy and Petrology, 80: 189？200.
[41]
Creaser R A, Price R C and Wormald R J. 1991. A-type granites revisited: Assessment of a residual-source model. Geology, 19: 163？ 166.
[42]
Eby G N. 1992. Chemical subdivision of the A-type granitoids: Petrogenetic and tectonic implications. Geology, 20: 641？644.
[43]
Harris C, Marsh J S and Milner S C. 1999. Petrology of the alkaline core of the messum igneous complex, Namibia: Evidence for the progressively decreasing effect of crustal contamination. Journal of Petrology, 40: 1377？1397.
[44]
Hoskin P W O and Schaltegger U. 2003. The composition of zircon and igneous and metamorphic petrogenesis. Reviews in Mineralogy and Geochemistry, 53(1): 27？62.
[45]
King P L, White A J R, Chappell B W and Allen C M. 1997. Characterization and origin of aluminous A-type granites from the Lachlan fold belt, southeastern Australia. Journal of Petrology, 38(3): 371？391.
[46]
Liégeois J P. 1998. Some words on the post-collisional magmatism. Lithos, 45: 15？18.
[47]
Liu Y S, Gao S, Hu Z C, Gao C G, Zong K Q and Wang D B. 2010. Continental and oceanic crust recycling-induced melt-peridotite interactions in the trans-North China Orogen: U-Pb dating, Hf isotopes and trace elements in zircons from mantle xenoliths. Journal of Petrology, 51(1？2): 537？571.
[48]
Liu Y S, Hu Z C, Gao S, Detlef Günther, Xu J, Gao C G and Chen H H. 2008. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard. Chemical Geology, 257(1？2): 34？43.
[49]
Ludwig K R. 2003. User’s Manual for Isoplot 3.00: A geochronological toolkit for Microsoft Excel. Berkeley Geochronology Center, Special Publication, 4: 1？70.
[50]
Middlemost E A K. 1994. Naming materials in the magma / igneous rock system. Earth Science Reviews, 37(3？4): 215？224.
[51]
Rapp R P and Watson E B. 1995. Dehydration melting of metabasalt at 8~32 kbar: Implications for continental growth and crust-mantle recycling. Journal of Petrology, 36: 891？931.
[52]
Rickwood P C. 1989. Boundary lines within petrologic diagrams which use oxides of minor elements. Lithos, 22: 247？263.
[53]
Skjerlie K P and Johnston A D. 1992. Vapor-absent melting at 10 kbar of a biotite- and amphibole-bearing tonalitic gneiss: Implications for the generation of A-type granites. Geology, 20: 263？266.
[54]
Streckeisen A L. 1976. Classification of the common igneous rocks by means of their chemical composition: A provisional attempt. Neues Jahrbuch für Mineralogie, Monatshefte, 1: 1？15.
[55]
Sun S S and McDonough W F. 1989. Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and processes // Saunders A D and Norry M J. Magmatism in Oceanic Basins. Geological Society, London, Special Publications, 42: 313？ 345.
[56]
Sylvester P J. 1989. Post-collisional alkaline granites. The Journal of Geology, 97: 261？280.
[57]
Taylor S R and McLennan S M. 1985. The Continental Crust: Its Composition and Evolution. London: Blackwell: 57？72.
[58]
Turner S P, Foden J D and Morrison R S. 1992. Derivation of some A-type magmas by fractionation of basaltic magma: An example from the Padthaway Ridge, South Australia. Lithos, 28: 151？179.
[59]
Whalen J B, Currie K L and Chappell B W. 1987. A-type granites: Geochemical characteristics, discrimination and petrogenesis. Contributions to Mineralogy and Petrology, 95: 407？419.
[60]
Whalen J B, Jenner G A, Longstaffe F J, Robert F and Gariepy C. 1996. Geochemical and isotopic (O, Nd, Pb and Sr) constraints on A- type granite: Petrogenesis based on the Topsails igneous suite, Newfoundland Appalachians. Journal of Petrology, 37: 1463？1489.
[61]
Yang J H, Wu F Y, Chung S L, Wilde S A and Chu M F. 2006. A hybrid origin for the Qianshan A-type granite, northeast China: Geochemical and Sr-Nd-Hf isotopic evidence. Lithos, 89: 89？106.
[62]
Yang J S, Robinson P T, Jiang C F and Xu Z Q. 1996. Ophiolites of the Kunlun Mountains, China and their tectonic implications. Tectonophysics, 258: 215？231
