Andersent T,Correction of common lead in U-Pb analyses that do not report 204Pb,Chemical Geology,2002.
[3]
Bievre D P,Taylor P D,Table of the isotopic compositions of the elements,International Journal of Mass Spectrometry and Ion Processes,1993(02).
[4]
Blank L P,Kamo S L,Williams I S,The application of SHRIMP to Phanerozoic geochronology:A critical appraisal of four zircon standards,Chemical Geology,2003.
[5]
Blichert-Toft J,Albarede F,The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle-crust system,Earth and Planetary Science Letters,1997.
[6]
Bureau of Geology and Mineral Resources of Xinjiang Uygur Autonomous Region,Regional geology of Xinjiang Uygur Autonomous Region,北京:地质出版社,1993.
[7]
Chen Y,Xu B,Zhan S,Li Y,First mid-Neoproterozoic paleomagnetic results from the Tarim Basin (NW China) and their geodynamic implications,Precambrian Research,2004.
[8]
Chu N C,Taylor R N,Chavagnac V,Hf isotope ratio analysis using multi-collector inductively coupled plasma mass spectrometry:An evaluation of isobaric interference corrections,Journal of Analytical Atomic Spectrometry,2002.
[9]
Cui J W,Guo X P,Ding X Z,Zhang X W,Mesozoic-Cenozoic deformation structures and their dynamics in the basin range junction belt of the west Kunlun Tarim basin (in Chinese with English Abstract),Earth Sciences Frontiers,2006(04).
[10]
Ding D G,Wang D X,Liu W X,West Kunlun oroginic belt and basin,北京:地质出版社,1999.
[11]
Jiang C F,Wang Z Q,Li J Y,Opening-Closing Tectonics of Central Orogenic Belt,北京:地质出版社,2000.
[12]
Ludwig K R,Isoplot 3.0-A geochronological toolkit for Micro-soft Excel,Berkeley Geochronology Center,2003.
[13]
Scherer E,Muenker C,Calibration of the lutetium-hafnium clock,Washington,DC:American Association for the Advancement of Science,2001.
[14]
Vervoort J D,Blichert-Toft J,Evolution of the depleted mantle:Hf isotope evidence from juvenile rocks through time,Geochimica Et Cosmochimica Acta,1999.
[15]
Xu B,Jiang P,Zheng H F,Zou H B,Zhang L F,Liu D Y,U Pb zircon geochronology of Neoproterozoic volcanic rocks in the Tarim Block of northwest China:implications for the breakup of Rodinia supercontinent and Neoproterozoic glaciations,Precambrian Research,2005.
[16]
Wang Y Z,The age and tectonic significance of the Yishake Group in West Kunlun (in Chinese with English Abstract),Xinjiang Geology,1983(01).
[17]
Wu F Y,Li X H,Zheng Y F,Gao S,Lu-Hf isotopic systimatics and their applications in petrology (in Chinese with English Abstract),Acta Petrologica Sinica,2007(02).
[18]
Yuan H L,Gao S,Dai M N,Simultaneous determinations of U-Pb age,Hf isotopes and trace element compositions of zircon by excimer laser ablation quadrupole and multiple collector ICP-MS,Chemical Geology,2008.
[19]
Zhang C L,Zhao Y,Guo K Y,Dong Y G Wang A G,Geochemistry Characteristics of the Proterozoic Meta-Basalt in Southern Tarim Plate:Evidence for the Meso-Proterozoic Breakup of Paleo-Tarim Plate (in Chinese with English Abstract),Earth Science-journal of China University of Geosciences,2003(01).
[20]
Zhang C L,Lu S N,Yu H F,Ye H M,Tectonic evolution of Western Orogenic belt:evidences from zircon SHRIMP and LA-ICP-MS U-Pb ages,Science in China(Series D),2007(02).
[21]
Zhang C L,Li Z X,Li X H,Ye H M,Neoproterozoic mafic dyke swarms at the northern margin of the Tarim Block,NW China:Age,geochemistry,petrogenesis and tectonic implications,Journal of Asian Earth Sciences,2009.
[22]
Zheng Y F.Zhang S B Formation and evolution of Precambrian continental crust in South China [J].-Chinese Science Bulletin2007(01)