Compston W,Williams I S,Kirschvink J L,Zircon U-Pb ages for the Early Cambrian time scale,Journal of the Geological Society(London),1992.
[18]
Harris N B W,Pearce J A,Tindle A G,Geochemical characteristics of collision-zone magmatism,1986.
[19]
Hoskin P W O,Black L P,Metamorphic zircon formation by solid-state recrystallization of protolith igneous zircon,Journal of Metamorphic Geology,2000.
[20]
Le Maitre R W,Bateman P,Dudek A,A Classification of Igneous Rocks and Glossary of Terms,Oxford:Blackwell Scientific Publications,1989.
[21]
Wood D A,Dynamic partial melting:Its application to the petrogenesis of basalta eruption in Iceland,the Faeroe Islands,the Isle of Skye (Scotland) and Troods Massif (Cyprus),Geochimica et Cosmochimica Acta,1979(07).
[22]
Yan Zhen,Wang Zongqi,Yan,Quanren Wang Tao,Devonian Sedimentary Environments and Provenance of the Qinling Orogen:Constraints on Late Paleozoic Southward Accretionary Tectonics of the North China Craton,International Geology Review,2006.
[23]
Zhihong Chen,Songnian Lu,Huaikun Li,Constraining the role of the Qinling orogen in the assembly and break-up of Rodinia:Tectonic implications for Neoproterozoic granite occurrences,Journal of Asian Earth Sciences,2006.
Ludwig K R,Isoplot/ Ex version 2.49.A Geochronological Toolkit for Microsoft Excel,Berkeley:Berkeley Geochronology Center,2003.
[27]
Mattauer M,Matte P,Malavieille J,Tectonics of the Qinling belt:build-up and evolution of eastern Asia,Nature,1985.
[28]
Meng Q R,Zhang G W,Geologic framework and tectonic evolution of Qingling orogen,Central China,Tectonophysics,2000.
[29]
Meng Q,Zhang G,Timing of collision of the North and South China blocks:controversy and reconciliation,Geology,1999.
[30]
Pearce A,Sources and settings of granitic rocks,Episodes,1996.
[31]
Turner S,Sandiford M,Foden J,Some geodynamic and compositional constraints on"postorogenic"magmatism,Geology,1998.
[32]
Wang Tao,Wang Xiaoxia,Zhang Guowei,Pei Xianzhi Zhang Chengli,Remnants of a Neoproterozoic collisional orogenic belt in the core of the Phanerozoic Qinling orogenic belt (China),Gondwana Research,2003(04).
[33]
Williams I S,Claesson S,Isotopic evidence for the Precambrian provenance and Caledonian metamorphism of high grade paragneisses from the Seve Nappes,Scandinavian Caledonides:II.Ion microprobe zircon U-Th-Pb,Contributions to Mineralogy & Petrology,1987.