Radhakrishna T and Joseph M. 1996. Proterozoic palaeomagnetism of the mafic dyke swarms in the high-grade region of southern India. Precambrian Research, 76: 31？46.
[23]
Shu L S, Zhou X M, Deng P, Wang B, Jiang S Y, Yu J H and Zhao X X. 2009. Mesozoic tectonic evolution of the Southeast China Block: New insights from basin analysis. Journal of Asian Earth Sciences, 34(3): 376？391.
[24]
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 the Ocean Basins. Geological Society, London, Special Publication, 42: 313？345.
[25]
Andersen Tom. 2002. Correction of common lead in U-Pb analyses that do not report 204Pb. Chemical Geology, 192: 59？79.
[26]
Wu F Y, Lin J Q, Wilde S A, Zhang X O and Yang J H. 2005. Nature and significance of the Early Cretaceous giant igneous event in eastern China. Earth and Planetary Science Letters, 233(1？2): 103？l19.
[27]
Zhang D, Liu W C, Wu G G, Li D X, Di Y J, Zang W S, Zhang X X and Huang H J. 2008. Magnetic abric and emplacement of the Fenghuangshan pluton, Tongling, Anhui Province, East-Central China. International Geology Review, 50(11): 994？1007.
[28]
Zhou X M, Sun T, Shen W Z, Shu L S and Niu Y L. 2006. Petrogenesis of Mesozoic granitoids and volcanic rocks in South China: A response to tectonic evolution. Episodes, 29(1): 26？33.
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: 602？622.
[41]
Faure M, Sun Y, Shu L, Monié P and Charvet J. 1996. Extensional tectonics within a subduction-type orogen: The case study of the Wugongshan dome (Jiangxi Province, southeastern China). Tectonophysics, 263: 77？106.
[42]
Hoek J D and Seitz H M. 1995. Continental mafic dyke swarms as tectonic indicators: An example from the Vestfold Hills, East Antarctica. Precambrian Research, 75(3？4): 121？139.
[43]
Hoffman P F. 1991. Did the breakout of Lauentia turn Gondwanaland inside-out? Science, 252: 1406？1412.
[44]
Irvine T N and Barager W R A. 1971. A guide to the chemical classification of the common volcanic rocks. Canadian Journal of Earth Sciences, 8: 532？548.
[45]
Le Bas M J, Maitre, R W, Strecklsen A and Zanettin B.1986. A chemical classification of volcanic rocks based on the total alkli-slica diagram. Journal of Petrology, 27(3): 745？750.
[46]
Li X H, Li W X, Wang X C, Li Q L, Liu Y, Tang G Q, Gao Y Y and Wu F Y. 2010. SIMS U-Pb zircon geochronology of porphyry Cu-Au-(Mo) deposits in the Yangtze River Metallogenic Belt, eastern China: Magmatic response to Early Cretaceous lithospheric extension. Lithos, 119: 427？438.
[47]
Li X H. 2000. Cretaceous magmatism and lithospheric extension in Southeast China. Journal of Asian Earth Science, 18: 293？305.
[48]
Ormerod D S, Hawkesworth C J, Rogers N W, Leeman W P and Menzies M A. 1988. Tectonic and magmatic transitions in the Western Great Basin, USA. Nature, 333(6171？6172): 349？353.
[49]
Pearce J A.1982.Trace element characteristics of lavas from destructive plate boundaries // Thorpe R S. Orogenic Andesites and Related Rocks. Wiley, New York: 525？548.
[50]
Peng P, Zhai M G, Ernst R, Guo J H, Liu F and Hu B. 2008. A 1.78 Ga Large Igneous Province in the North China Craton: The Xiong’er Volcanic Province and the North China dyke swarm. Lithos, 101(3？4): 260？280.
