Batchelor R A and Bowden P. 1985. Petrogenetic interpretation of granito id rock series using multicationic parameters[J]. Chemical Geology, 48(1-4): 43-55.
[21]
更多...
[22]
Boynton W V. 1984. Geochemistry of the rare earth elements: Meteorite studies[A]. In: Henderson P, ed. Rare earth element geochemistry[C]. Amsterdam: E lsevier Press. 63-114.
[23]
Chappell B W and White A J R. 1974. Two contrasting granite types[J]. Pacific Geology, 8: 173-174.
[24]
Chappell B W and White A J R. 1992. I-and S-type granites in the Lachlan Fold B elt[J]. Transactions of the Royal Society of Edinburgh: Earth Sciences, 83(1-2 ): 1-26.
[25]
Chappell B W. 1999. Aluminium saturation in I-and S-type granites and the chara cterization of fractionated haplogranites[J]. Lithos, 46(3): 535-551.
[26]
Chappell B W and White A J R. 2001. Two contrasting granite types: 25 years late r[J]. Australian Journalof Earth Sciences, 48(4): 489-499.
[27]
Eby G N. 1990. The A-type granitoids: A review of their occurrence and chemical characteristics and speculation on their petrogenesis[J]. Lithos, 26(1-2): 115 -134.
[28]
King P L, Chappell B W, Allen C M and White A J R. 2001. Are A-type granites the high-temperature felsic granites? Evidence from fractionated granites of the Wa ngrah Suite[J]. Australian Journal of Earth Sciences, 48(4): 501-514.
[29]
Li X H, Li Z X, Li W X, Liu Y, Yuan C, Wei G J and Qi C S. 2007. U-Pb zircon, ge ochemical and Sr-Nd-Hf isotopic constraints on age and origin of Jurassic I-and A-type granites from central Guangdong, SE China: A major igneous event in respo nse to foundering of a subducted flat-slab[J]. Lithos, 96(1-2): 186-204.
[30]
McDonough W F and Sun S S. 1995. The composition of the Earth[J]. Chemical Geo logy, 120: 223-253.
[31]
Middlemost E A K. 1994. Naming materials in the magma/igneous rock system[J]. Earth-Science Reviews, 37(3-4): 215-244.
[32]
Rollisonhr H R. 1993. Using geochemical data: Evaluation, presentation, interpre tation[M]. London: Longman Group UK Ltd.
[33]
Turner S, Arnaud N, Liu J, et al. 1996. Post-collision, shoshonitic volcanism on the Tibetan Plateau: Implications for convective thinning of the lithosphere an d the source of ocean island basalts[J]. Petrology, 37 (1): 45-71.
[34]
Whalen J B, Currie K L and Chappell W. 1987. A-type granites: Geochemical charac teristics, discrimination and petrogenesis[J]. Contributions to Mineralogy and Petrology, 95(4): 407-419.
[35]
Wu F Y, Jahn B M, Wilde S A, Lo C H, Yui T F, Lin Q, Ge W C and Sun D Y. 2003. H ighly fractionated I-type granites in NE China (I): Geochronology and petrogenes is[J]. Lithos, 66(3-4): 241-273.
[36]
Xue H M, Dong S W and Liu X C. 2001. Geochemical characteristics and their genes is of the granitic gneisses from Southeastern Dabie Mountain[J]. Acta Geologic a Sinca, 14(2): 175-183.
[37]
Xue H M, Wang Y G, Ma F, Wang C, Wang D E and Zuo Y L. 2009. Zircon U-Pb SHRIMP ages of the Taiping (calc-alkaline) -Huangshan (alkaline) composite intrusive: C onstraints on Mesozoic lithospheric thinning of the southeastern Yangtze craton [J]. Sci. China (Ser. D), 39(7): 979-993.
