Andersen T. 2002. Correction of common lead in U-Pb analyses that do not report 204Pb. Chemical Geology, 192(1): 59-79.
[14]
Chen B, Jahn B M and Tian W. 2009. Evolution of the Solonker suture zone: Constraints from zircon U-Pb ages, Hf isotopic ratios and whole-rock Nd-Sr isotope compositions of subduction- and collision-related mag?mas and forearc sediments. Journal of Asian Earth Sciences, 34(3): 245-257.
[15]
Cohen K M, Finney S C and Gibbard P L. 2013. The ICS international chronostratigraphic chart. Episodes, 36(3): 199-204.
[16]
Diwu C, Sun Y, Yuan H, Wang H, Zhong X and Liu X. 2008. U-Pb ages and Hf isotopes for detrital zircons from quartzite in the Paleoproterozoic Songshan Group on the southwestern margin of the North China Craton. Chinese Science Bulletin, 53(18): 2828-2839.
[17]
Wang H and Liu X Y. 1986. Paleoplate tectonics between Cathasia and Angaraland in Inner Mongolia of China. Tectonics, 5(7): 1073-1088.
[18]
Wang Y, Zhang F Q, Zhang D W, Miao L C, Li T S, Xie H Q, Meng Q R and Liu D Y. 2006. Zircon SHRIMP U-Pb dating of meta-diorite from the basement of the Songliao Basin and its geological significance. Chinese Science Bulletin, 51(15): 1877-1883.
[19]
Wu F Y, Sun D Y, Ge W C, Zhang Y B, Grantc M L, Wildec S A and Jahnd B M. 2011. Geochronology of the Phanerozoic granitoids in northeastern China. Journal of Asian Earth Sciences, 41: 1-30.
[20]
Xiao W J, Windley F B, Hao J and Zhai M G. 2003. Accretion leading to collision and the Permian Solonker suture, Inner Mongolia, China: Termination of the central Asian orogenic belt. Tectonics, 22(6): 8-17
[21]
Yuan H L, Gao S, Dai M N, Zong C L, Günther D, Fontaine G H, Liu X M and Diwu C. 2008. Simultaneous determinations of U-Pb age, Hf isotopes and trace element compositions of zircon by excimer laser-abl?ation quadrupole and multiple-collector ICP-MS. Che?mical Geology, 247(1): 100-118.
[22]
Zhang X H, Zhang H F, Tang Y J, Wilde S A and Hu Z C. 2008. Geochemistry of Permian bimodal volcanic rocks from central Inner Mongolia, North China: Implication for tectonic setting and Phanerozoic continental growth in Central Asian Orogenic Belt. Chemical Geology, 249(3): 262-281.
[23]
Zhou J B and Wilde S A. 2013. The crustal accretion history and tectonic evolution of the NE China segment of the Central Asian Orogenic Belt. Gondwana Research, 23: 1365-1377.
[24]
Zhou J B, Wilde S A, Zhang X Z, Zhao G C, Zheng C Q, Wang Y J and Zhang X H. 2009. The onset of Pacific margin accretion in NE China: Evidence from the Heilongjiang high-pressure metamorphic belt. Tecton?op?hysics, 478: 230-246.
[25]
Zhou J B, Wilde S A, Zhao G C, Zhang X Z, Wang H and Zeng W S. 2010a. Was the easternmost segment of the Central Asian Orogenic Belt derived from Gondwana or Siberia: An intriguing dilemma. Journal of Geodyna?mics, 50(3): 300-317.
[26]
Zhou J B, Wilde S A, Zhao G C, Zhang X Z, Zheng C Q, Wang H and Zeng W S. 2010b. Pan-African metamo?rphic and magmatic rocks of the Khanka Massif, NE China: Further evidence regarding their affinity. Ge?ological Magazine, 147(5): 737-749.
[27]
Zhu Y F, Sun S H, Gu L B, Ogasawara Y, Jiang N and Honma H. 2001. Permian volcanism in the Mongolian orogenic zone, northeast China: Geochemistry, magma sources and petrogenesis. Geological Magazine 138(2): 101-115.
Guo F, Fan W M, Li C W, Miao L C and Zhao L. 2009. Early Paleozoic subduction of the Paleo-Asian Ocean: Geochronological and geochemical evidence from the Dashizhai basalts, Inner Mongolia. Science in China (Series D), 52: 940-951.
[51]
Hoskin P W O and Black L P. 2000. Metamorphic zircon formation by solid-state recrystallization of protolithi?gneous zircon. Journal of Metamorphic Geology, 18(4): 423-439.
[52]
Jian P, Liu D Y, Kr?ner A, Windley B F, Shi Y R, Zhang F Q, Miao L C, Zhang Q, Zhang L Q and Ren J S. 2008. Time scale of an early to mid-Paleozoic orogenic cycle of the long-lived Central Asian Orogenic Belt, Inner Mongolia of China: Implications for continental growth. Lithos, 101: 233-259.
[53]
Li J Y. 2006. Permian geodynamic setting of northeast China and adjacent regions: Closure of the Paleo-Asian Ocean and subduction of the Paleo-Pacific plate. Journal of Asian Earth Sciences, 26: 207-224.
[54]
Liégeois J P. 1998. Preface-Some words on the post-coll?isional magmatism. Lithos, 45: xv-xvii.
[55]
Miao L C, Fan W M, Liu D Y, Zhang F Q, Shi Y R and Guo F. 2008. Geochronology and geochemistry of the Hege?n?shan ophiolitic complex: Implications for late-stage tectonic evolution of the Inner Mongolia-Daxinganling Orogenic Belt, China. Journal of Asian Earth Sciences, 32(5-6): 348-370.
[56]
Miao L C, Liu D Y, Zhang F Q, Fan W M, Shi Y R and Xie H Q. 2007. Zircon SHRIMP U-Pb ages of the “Xingh?ua-dukou Group” in Hanjiayuanzi and Xinlin areas and the “Zhalantun Group” in Inner Mongolia, Da Hinggan Mountains. Chinese Science Bulletin, 52(8): 1112-1124.
[57]
Pei F P, Xu W L, Yang D B, Zhao Q G, Liu X M and Hu Z C. 2007. Zircon U-Pb geochronology of basement metam-orphic rocks in the Songliao Basin. Chinese Science Bulletin, 52(7): 942-948.
[58]
Shi G H, Liu D Y, Zhang F Q, Jian P, Miao L C, Shi Y R and Tao H. 2003. SHRIMP U-Pb zircon geochronology and its implications on the Xilin Gol Complex, Inner Mongolia, China. Chinese Science Bulletin, 48(24): 2742-2748.
[59]
Sorokin A A, Kudryashov N M, Li J Y, Zhuravlev D Z, Pin Y, Sun G H and Gao L M. 2004. Early Paleozoic granit?oids in the eastern margin of the Argun''terrane, Amur area: First geochemical and geochronologic data. Petrology, 12(4): 367-376.