1 Seng？r A M C, Natal'in B A, Burtman V S. Evolution of the Altaid tectonic collage and Paleozoic crustal growth in Eurasia. Nature, 1993, 364: 299-307
[2]
2 Windley B F, Alexeiev D, Xiao W J, et al. Tectonic models for accretion of the Central Asian Orogenic Belt. J Geol Soc, London, 2007, 164: 31-47
[3]
5 Ge R F, Zhu W B, Wilde S A, et al. Neoproterozoic to Paleozoic long-lived accretionary orogeny in the northern Tarim Craton. Tectonics, 2014, 33, doi: 10.1002/2013TC003501
[4]
6 Levashova N M, Meert J G, Gibsher A S, et al. The origin of microcontinents in the Central Asian orogenic belt: Constraints frompaleomagnetism and geochronology. Precambrian Res, 2011, 185: 37-54
[5]
7 Wilhem C, Windley B F, Stampfli G M. The Altaids of Central Asia: A tectonic and evolutionary innovative review. Earth-Sci Rev, 2012, 113: 303-341
[6]
8 Salnikova E, Kozakov I, Kotov A, et al. Age of Palaeozoic granites and metamorphism in the Tuvino-Mongolian Massif of the Central Asian Mobile Belt: Loss of a Precambrian microcontinent. Precambrian Res, 2001, 110: 143-164
[7]
9 Sun M, Yuan C, Xiao W, et al. Zircon U-Pb and Hf isotopic study of gneissic rocks from the Chinese Altai: Progressive accretionary history in the early to middle Palaeozoic. Chem Geol, 2008, 247: 352-383
[8]
10 Song D, Xiao W, Han C, et al. Progressive accretionary tectonics of the Beishan orogenic collage, Southern Altaids: Insights from zircon U-Pb and Hf isotopic data of high-grade complexes. Precambrian Res, 2012, 227: 368-388
[9]
11 Long X, Sun M, Yuan C, et al. Detrital zircon age and Hf isotopic studies for metasedimentary rocks from the Chinese Altai: Implications for the Early Paleozoic tectonic evolution of the Central Asian Orogenic Belt. Tectonics, 2007, 26: TC5015
[10]
12 He Z Y, Zhang Z M, Zong K Q, et al. Zircon U-Pb and Hf isotopic studies of the Xingxingxia Complex from Eastern Tianshan (NW China): Significance to the reconstruction and tectonics of the southern Central Asian Orogenic Belt. Lithos, 2014, 190: 485-499
[11]
13 Huang B T, He Z Y, Zhang Z M, et al. Early Neoproterozoic granitic gneisses in the Chinese Eastern Tianshan: Petrogenesis and tectonic implications. J Asian Earth Sci, 2014, http://dx.doi.org/10.1016/j.jseaes.2014.08.021
[12]
14 Kr？ner A, Kovach V, Belousova E, et al. Reassessment of continental growth during the accretionary history of the Central Asian Orogenic Belt. Gondwana Res, 2014, 25: 103-125
[13]
15 Cleven N R, Lin S, Xiao W. The Hongliuhe fold-and-thrust belt: Evidence of terminal collision and suture-reactivation after the Early Permian in the Beishan orogenic collage, Northwest China. Gondwana Res, 2015, 27: 796-810
[14]
16 Tian Z, Xiao W, Windley B F, et al. Structure, age, and tectonic development of the Huoshishan-Niujuanzi ophiolitic mélange, Beishan, southernmost Altaids. Gondwana Res, 2014, 25: 820-841
[15]
19 Shi W X, Liao Q A, Hu Y Q, et al. Characteristics of Mesoproterozoic granites and their geological significances from Middle Tianshan Block, East Tianshan district, NW China (in Chinese). Geol Sci Technol Inform, 2010, 29: 29-37 [施文翔, 廖群安, 胡远清, 等. 东天山地区中天山地块内中元古代花岗岩的特征及地质意义. 地质科技情报, 2010, 29: 29-
[16]
20 Ye X F, Zong K Q, Zhang Z M, et al. Geochemistry of Neoproterozoic granite in Liuyuan area of southern Beishan orogenic belt and its geological significance (in Chinese). Geol Bull China, 2013, 32: 307-317 [叶晓峰, 宗克清, 张泽明, 等. 北山造山带南缘柳园地区新元古代花岗岩的地球化学特征及其地质意义. 地质通报, 2013, 32: 307-
[17]
21 Jiang H Y, He Z Y, Zong K Q, et al. Zircon U-Pb dating and Hf isotopic studies on the Beishan complex in the southern Beishan orogenic belt (in Chinese). Acta Petrol Sin, 2013, 29: 3949-3967 [姜洪颖, 贺振宇, 宗克清, 等. 北山造山带南缘北山杂岩的锆石U-Pb定年和Hf同位素研究. 岩石学报, 2013, 29: 3949-
[18]
22 He Z Y, Zhang Z M, Zong K Q, et al. Paleoproterozoic crustal evolution of the Tarim Craton: Constrained by zircon U-Pb and Hf isotopes of meta-igneous rocks from Korla and Dunhuang. J Asian Earth Sci, 2013, 78: 54-70
[19]
23 Zong K, Liu Y, Zhang Z, et al. The generation and evolution of Archean continental crust in the Dunhuang block, northeastern Tarim craton, northwestern China. Precambrian Res, 2013, 235: 251-263
[20]
24 Wang Z M, Han C M, Xiao W J, et al. The petrogenesis and tectonic implications of the granitoid gneisses from Xingxingxia in the eastern segment of Central Tianshan. J Asian Earth Sci, 2014, 88: 277-292
[21]
25 Huang B T, He Z Y, Zong K Q, et al. 2014. Zircon U-Pb and Hf isotopic study of Neoproterozoic granitic gneisses from the Alatage area: Constraints on the Precambrian crustal evolution in the Chinese Central Tianshan Block. Chin Sci Bull, 2014, 59: 100-112
[22]
33 Mei H L, Li H M, Lu S N, et al. The age and origin of the Liuyuan granitoid, Northwestern Gansu (in Chinese). Acta Petrol Mineral, 1999, 18: 14-17 [梅华林, 李惠民, 陆松年, 等. 甘肃柳园地区花岗质岩石时代及成因. 岩石矿物学杂志, 1999, 18: 14-
[23]
34 Qu J F, Xiao W J, Windley B F, et al. Ordovician eclogites from the Chinese Beishan: Implications for the tectonic evolution of the southern Altaids. J Metamorph Geol, 2011, 29: 803-820
[24]
35 Mei H L, Yu H F, Li Q, et al. The first discovery of eclogite and Palaeoproterozoic grantiods in the Beishan area, northwestern Gansu Province, China (in Chinese). Chin Sci Bull, 1998, 43: 2105-2111 [梅华林, 于海峰, 李铨, 等. 甘肃北山地区首次发现榴辉岩和古元古花岗质岩石．科学通报, 1998, 43: 2105-
[25]
36 Zuo G C, Zhang S L, He G Q, et al. Early Paleozoic plate tectonics in Beishan area (in Chinese). Sci Geol Sin, 1990, 4: 305-314 [左国朝, 张淑玲, 何国琦, 等. 北山地区早古生代板块构造特征. 地质科学, 1990, 4: 305-
[26]
37 Zuo G C, Liu Y K, Liu C Y. Framework and evolution of the tectonic structure in Beishan area across Gansu Province, Xinjiang Autonomous Region and Inner Mongolia Autonomous Region (in Chinese). Acta Geol Gansu, 2003, 12: 1-15 [左国朝, 刘义科, 刘春燕. 甘新蒙北山地区构造格局及演化. 甘肃地质学报, 2003, 12: 1-
[27]
39 Li S, Wang T, Tong Y, et al. Identification of the Early Devonian Shuangfengshan A-type granites in Liuyuan area of Beishan and its implications to tectonic evolution (in Chinese). Acta Petrol Mineral, 2009, 28: 407-422 [李舢, 王涛, 童英, 等. 北山柳园地区双峰山早泥盆世 A 型花岗岩的确定及其构造演化意义. 岩石矿物学杂志, 2009, 28: 407-
[28]
44 Ludwig K R. Users Manual for Isoplot/Ex (rev. 2.49): A geochronological toolkit for microsoft excel. Berkeley Geochronology Center, Special Publication, 2001, No. 1a, 55
[29]
45 Scherer E, Munker C, Mezger K. Calibration of the Lutetium-Hafnium Clock. Science, 2001, 293: 683-687
[30]
46 Bouvier A, Vervoort J D, Patchett P J. The Lu-Hf and Sm-Nd isotopic composition of CHUR: Constraints from unequilibrated chondrites and implications for the bulk composition of terrestrial planets. Earth Planet Sci Lett, 2008, 273: 48-57
[31]
47 Griffin W L, Pearson N J, Belousova E, et al. The Hf isotope composition of cratonic mantle: LAM-MC-ICPMS analysis of zircon megacrysts in kimberlites. Geochim Cosmochim Acta, 2000, 64: 133-147
[32]
48 Wu F Y, Yang Y H, Xie L W, et al. Hf isotopic compositions of the standard zircons and baddeleyites used in U-Pb geochronology. Chem Geol, 2006, 234: 105-126
[33]
49 Rubatto D, Gebauer D. Use of cathodoluminescence for U-Pb zircon dating by ion microprobe: Some examples from the Western Alps. In: Pagel M, Barbin V, Blance P, et al, eds. Cathodoluminescence in Geosciences. Berlin, Heidelberg: Springer-Verlag, 2000. 373-400
[34]
50 Zhang J X, Yu S Y, Gong J H, et al. The latest Neoarchean-Paleoproterozoic evolution of the Dunhuang block, eastern Tarim Craton, northwestern China: Evidence from zircon U-Pb dating and Hf isotopic analyses. Precambrian Res, 2013, 226: 21-42
[35]
51 Zheng Y F, Zhang S B, Zhao Z F, et al. Contrasting zircon Hf and O isotopes in the two episodes of Neoproterozoic granitoids in South China: Implications for growth and reworking of continental crust. Lithos, 2007, 96: 127-150
[36]
52 Humphreys M C, Blundy J D, Sparks R S J. Magma evolution and open-system processes at Shiveluch Volcano: Insights from phenocryst zoning. J Petrol, 2006, 47: 2303-2334
[37]
56 Peng M X, Zhong C G, Zuo Q H, et al. The ages of the gneissic granite from Kawabulag area in the Eastern Tianshan and their geological significances (in Chinese). Xinjiang Geol, 2012, 30: 12-18 [彭明兴, 钟春根, 左琼华, 等. 东天山卡瓦布拉克地区片麻状花岗岩形成时代及地质意义. 新疆地质, 2012, 30: 12-
[38]
3 Xiao W, Windley B, Huang B, et al. End-Permian to mid-Triassic termination of the accretionary processes of the southern Altaids: Implications for the geodynamic evolution, Phanerozoic continental growth, and metallogeny of Central Asia. Int J Earth Sci, 2009, 98: 1189-1217
[39]
4 Xiao W J, Mao Q G, Windley B F, et al. Paleozoic multiple accretionary and collisional processes of the Beishan orogenic collage. Am J Sci, 2010, 310: 1553-1594
[40]
17 Hu A Q, Wei G J, Deng W F, et al. 1.4 Ga SHRIMP U-Pb age for zircons of granodiorite and its geological significance from the eastern segment of the Tianshan Mountains, Xinjiang, China (in Chinese). Geochimica, 2006, 35: 333-345 [胡霭琴, 韦刚健, 邓文峰, 等. 天山东段1.4 Ga花岗闪长质片麻岩SHRIMP锆石U-Pb年龄及其地质意义. 地球化学, 2006, 35: 333-
[41]
18 Hu A Q, Wei G J, Jahn B M, et al. Formation of the 0.9 Ga Neoproterozoic granitoids in the Tianshan Orogen, NW China: Constraints from the SHRIMP zircon age determination and its tectonic significance (in Chinese). Geochemica, 2010, 39: 197-212 [胡霭琴, 韦刚健, 江博明, 等. 天山0.9 Ga新元古代花岗岩SHRIMP锆石U-Pb年龄及其构造意义. 地球化学, 2010, 39: 197-
[42]
26 Geological Survey of Gansu Province. Geological Map of Yumenzhen sheet, People's Republic of China (1:250000) (in Chinese). 2005 [甘肃省地质调查院. 中华人民共和国地质图玉门镇幅(1:250000).
[43]
27 He Z Y, Zong K Q, Jiang H Y, et al. Early Paleozoic tectonic evolution of the southern Beishan orogenic collage: Insights from the granitoids (in Chinese). Acta Petrol Sin, 2014, 30: 3949-3967 [贺振宇, 宗克清, 姜洪颖, 等. 北山造山带南部早古生代构造演化: 来自花岗岩的约束. 岩石学报, 2014, 30: 3949-
[44]
28 Konopelko D, Kullerud K, Apayarov F, et al. SHRIMP zircon chronology of HP-UHP rocks of the Makbal metamorphic complex in the Northern Tien Shan, Kyrgyzstan. Gondwana Res, 2012, 22: 300-309
[45]
29 Cawood P A, Nemchin A A, Strachan R, et al. Sedimentary basin and detrital zircon record along East Laurentia and Baltica during assembly and breakup of Rodinia. J Geol Soc, London, 2007, 164: 257-275
[46]
30 Kuznetsov N, Natapov L, Belousova E, et al. Geochronological, geochemical and isotopic study of detrital zircon suites from late Neoproterozoic clastic strata along the NE margin of the East European Craton: Implications for plate tectonic models. Gondwana Res, 2010, 17: 583-601
[47]
31 Liu X Y, Wang Q. Tectonics of orogenic belts in Beishan MTS, Western China and their evolution (in Chinese). Geosci Res, 1995, 28: 7-48 [刘雪亚, 王荃. 中国西部北山造山带的大地构造及其演化. 地学研究, 1995, 28: 7-
[48]
32 Liu X C, Chen B L, Jahn B M, et al. Early Paleozoic (ca. 465 Ma) eclogites from Beishan (NW China) and their bearing on the tectonic evolution of the southern Central Asian Orogenic Belt. J Asian Earth Sci, 2010, 42: 715-731
[49]
38 Zhao Z H, Guo Z J, Wang Y. Geochronology, geochemical characteristics and tectonic implications of the granitoids from Liuyuan area, Beishan, Gansu Province, northwest China (in Chinese). Acta Petrol Sin, 2007, 23: 1847-1860 [赵泽辉, 郭召杰, 王毅．甘肃北山柳园地区花岗岩类的年代学、地球化学特征及构造意义. 岩石学报, 2007, 23: 1847-
[50]
40 Mao Q, Xiao W, Fang T, et al. Late Ordovician to early Devonian adakites and Nb-enriched basalts in the Liuyuan area, Beishan, NW China: Implications for early Paleozoic slab-melting and crustal growth in the southern Altaids. Gondwana Res, 2012, 22: 534-553
[51]
41 Mei H L, Yu H F, Li T, et al. Preliminary litho-tectonic framework of early Precambrian rocks in Dunhuang-Beishan area, Gansu, west China (in Chinese). Progr Precambrian Res, 1997, 20: 47-54 [梅华林, 于海峰, 李铨, 等. 甘肃敦煌-北山早前寒武纪岩石组合-构造初步框架. 前寒武纪研究进展, 1997, 20: 47-
[52]
42 Chen B L, Wu G G, Yang N, et al. Baidunzi-Xiaoxugong ductile shear zone and its ore-controlling effect in the southern Beishan area, Gansu (in Chinese). J Geomechan, 2007, 13: 99-109 [陈柏林, 吴淦国, 杨农, 等. 甘肃北山白墩子-小西弓韧性剪切带及其控矿作用. 地质力学学报, 2007, 13: 99-
[53]
43 He Z Y, Xu X S, Zou H B, et al. Geochronology, petrogenesis and metallogeny of Piaotang granites in the tungsten deposit region of South China. Geochem J, 2010, 44: 299-313
[54]
53 Shaw S, Flood R. Zircon Hf isotopic evidence for mixing of crustal and silicic mantle-derived magmas in a zoned granite pluton, eastern Australia. J Petrol, 2009, 50: 147-168
[55]
54 Lu S, Li H, Zhang C, et al. Geological and geochronological evidence for the Precambrian evolution of the Tarim Craton and surrounding continental fragments. Precambrian Res, 2008, 160: 94-107
[56]
55 Chen X Y, Wang Y J, Sun L H, et al. Zircon SHRIMP U-Pb dating of the granitic gneisses from Bingdaban and Laerdundaban (Tianshan Orogen) and their geological significances (in Chinese). Geochemica, 2009, 38: 424-431 [陈新跃, 王岳军, 孙林华, 等. 天山冰达坂和拉尔敦达坂花岗片麻岩SHRIMP锆石年代学特征及其地质意义. 地球化学, 2009, 38: 424-
