1 Belousova E A, Reid A J, Griffin W L. Rejuvenation vs. Recycling of Archean crust in the gawler craton, south Australia: Evidence from U-Pb and Hf isotopes in detrital zircon. Lithos, 2009, 113: 570-582
[2]
3 Iizuka T, Komiya T, Rino S, et al. Detrital zircon evidence for Hf isotopic evolution of granitoid crust and continental growth. Geochim Cosmochim Acta, 2010, 74: 2450-2472
[3]
6 Zhai M G, Guo J H, Liu W J. Neoarchean to Paleoproterozoic continental evolution and tectonic history of the North China Craton: A review. J Asian Earth Sci, 2005, 24: 547-561
[4]
9 Zhao G C, Cawood P A, Wilde S A. Metamorphism of basement rocks in the central zone of the North China Craton: Implications for paleoproterozoic tectonic evolution. Precambrian Res, 2000, 103: 55-88
16 Yang C H, Du L L, Ren L D. SHRIMP U-Pb ages and stratigraphic correlation of the Angou group on the southern margin of the North China Craton. Acta Petrol Sin, 2009, 25: 1853-1862
18 Liu C H, Zhao G C, Sun M, et al. Detrital zircon U-Pb dating, Hf isotopes and whole-rock geochemistry from the Songshan group in the Dengfeng complex: Constraints on the tectonic evolution of the Trans-North China Orogen. Precambrian Res, 2012, 192-195: 1-15
[10]
19 Peng P, Zhai M G, Ernst R E, et al. A 1.78 Ga large igneous province in the North China Craton: The Xiong'er volcanic Province and the north China dyke swarm. Lithos, 2008, 101: 260-280
[11]
20 陕西省地质矿产局. 陕西区域地质志. 北京: 地质出版社, 1989. 1-698
[12]
21 Wang X L, Jiang S Y, Dai B Z. Melting of enriched archean subcontinental lithospheric mantle: Evidence from the ca. 1760 Ma volcanic rocks of the Xiong'er Group, southern margin of the North China Craton. Precambrian Res, 2010, 182: 204-216
[13]
22 Zhao G C, He Y H, Sun M, et al. The Xiong'er volcanic belt at the southern margin of the North China Craton: Petrographic and geochemical evidence for its outboard position in the Paleo-mesoproterozoic Columbia supercontinent. Gondwana Res, 2009, 16: 170-181
[14]
24 Chu N C, Taylor R N, Chavagnac V R, et al. Hf isotope ratio analysis using multi-collector inductively coupled plasma mass spectrometry: An evaluation of isobaric. J Anal Atom Spectrom, 2002, 17: 1567-1574
[15]
27 Vervoort J D, Blichert-Toft J. Evolution of the depleted mantle: Hf isotope evidence from juvenile rocks through time. Geochim Cosmochim Acta, 1999, 63: 533-556
[16]
28 Rudnick R L, Gao S. 3.01-composition of the continental crust. In: Treatise on Geochemistry. Oxford: Pergamon, 2003. 1-64
[17]
30 Andersen T. Detrital zircons as tracers of sedimentary provenance: Limiting conditions from statistics and numerical simulation. Chem Geol, 2005, 216: 249-270
[18]
31 Liu C H, Zhao G C, Sun M, et al. U-Pb and Hf isotopic study of detrital zircons from the hutuo group in the Trans-North China Orogen and tectonic implications. Gondwana Res, 2011, 20: 106-121
[19]
32 Liu C H, Zhao G C, Sun M, et al. U-Pb geochronology and Hf isotope geochemistry of detrital zircons from the Zhongtiao complex: Constraints on the tectonic evolution of the Trans-North China Orogen. Precambrian Res, 2012, 222-223: 159-172
[20]
41 Zhao G C, Wilde S A, Cawood P A, et al. SHRIMP U-Pb zircon ages of the Fuping complex: Implications for Late Archean to Paleoproterozoic accretion and assembly of the North China Craton. Am J Sci, 2002, 302: 191-226
[21]
42 Guan H, Sun M, Wilde S A, et al. Shrimp U-Pb zircon geochronology of the Fuping complex: Implications for formation and assembly of the North China Craton. Precambrian Res, 2002, 113: 1-18
51 Wang Z H, Wilde S A, Wan J L. Tectonic setting and significance of 2.3-2.1 Ga magmatic events in the Trans-North China Orogen: New constraints from the Yanmenguan mafic ultramafic intrusion in the Hengshan-Wutai-Fuping area. Precambrian Res, 2003, 178: 27-42
57 Condie K C, Aster R C. Episodic zircon age spectra of orogenic granitoids: The supercontinent connection and continental growth. Precambrian Res, 2010, 180: 227-236
60 Valley J W, Lackey J S, Cavosie A J, et al. 4.4 billion years of crustal maturation: Oxygen isotope ratios of magmatic zircon. Contrib Mineral Petrol, 2005, 150: 561-580
2 Wan Y S, Liu D Y, Wang W, et al. Provenance of Meso-Neoproterozoic cover sediments at the ming tombs, Beijing, North China Craton: An integrated study of U-Pb dating and Hf isotopic measurement of detrital zircons and whole-rock geochemistry. Gondwana Res, 2011, 20: 219-242
[33]
4 Hawkesworth C J, Dhuime B, Pietranik A B, et al. The generation and evolution of the continental crust. J Geol Soc London, 2010, 167: 229-248
7 Kusky T M, Li J H. Paleoproterozoic tectonic evolution of the North China Craton. J Asian Earth Sci, 2003, 22: 383-397
[36]
8 Kusky T M, Li J H, Tucker R D. The Archean Dongwanzi ophiolite complex, North China Craton: 2.505-billion-year-old oceanic crust and mantle. Science, 2001, 292: 1142-1145
[37]
10 Zhao G C, Sun M, Wilde S A, et al. Late archean to paleoproterozoic evolution of the North China Craton: Key issues revisited. Precambrian Res, 2005, 136: 177-202
[38]
13 Sun Y, Yu Z P, Kr?ner A. Geochemistry and single zircon geochronology of archaean TTG gneisses in the Taihua high-grade terrain, Lushan area, central China. J Southeast Asian Earth Sci, 1994, 10: 227-233
[39]
14 Zhang G W, Bai Y B, Sun Y, et al. Composition and evolution of the archaean crust in central Henan China. Precambrian Res, 1985, 27: 7-35
[40]
15 Diwu C R, Sun Y, Guo A L, et al. Crustal growth in the North China Craton at similar to 2.5 Ga: Evidence from in situ zircon U-Pb ages, Hf isotopes and whole-rock geochemistry of the Dengfeng complex. Gondwana Res, 2011, 20: 149-170
[41]
23 Ludwing K R. User's manual for isoplot 3.00: A geochronological toolkit for microsoft excel. Berkeley Geochronology Center, Special Publications, 2003. 1-71
[42]
25 Albarède F, Scherer E E, Blichert-Toft J, et al. Γ-ray irradiation in the early solar system and the conundrum of the 176Lu decay constant. Geochim Cosmochim Acta, 2006, 70: 1261-1270
[43]
26 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
33 Liu C H, Zhao G C, Sun M, et al. U-Pb and Hf isotopic study of detrital zircons from the Yejishan group of the Lüliang Complex: Constraints on the timing of collision between the eastern and western blocks, North China Craton. Sediment Geol, 2011, 236: 129-140
[46]
34 Liu D Y, Wilde S A, Wan Y S, et al. Combined U-Pb, Hafnium and oxygen isotope analysis of zircons from meta-igneous rocks in the southern North China Craton reveal multiple events in the late Mesoarchean-early Neoarchean. Chem Geol, 2009, 261: 140-154
36 Cui M L, Zhang B L, Zhang L C. U-Pb dating of baddeleyite and zircon from the Shizhaigou diorite in the southern margin of North China Craton: Constrains on the timing and tectonic setting of the Paleoproterozoic Xiong'er group. Gondwana Res, 2011, 20: 184-193
[49]
37 Kr?ner A, Wilde S A, Li J H, et al. Age and evolution of a late Archean to Paleoproterozoic upper to lower crustal section in the Wutaishan/Hengshan/Fuping terrain of Northern China. J Asian Earth Sci, 2005, 24: 577-595
40 王凯怡, Wilde S. 山西五台地区大洼梁花岗岩的SHRIMP锆石U-Pb精确年龄. 岩石矿物学杂志, 2002, 407: 411-420
[53]
44 Zhao G C, Wilde S A, Sun M, et al. Shrimp U-Pb zircon ages of granitoid rocks in the Lüliang complex: Implications for the accretion and evolution of the Trans-North China Orogen. Precambrian Res, 2008, 160: 213-226
48 Liu S W, Zhang J, Li Q G, et al. Geochemistry and U-Pb zircon ages of metamorphic volcanic rocks of the Paleoproterozoic Lüliang complex and constraints on the evolution of the Trans-North China Orogen, North China Craton. Precambrian Res, 2012, 222-223: 173-190
[57]
50 Peng P, Guo J H, Zhai M G, et al. Genesis of the Hengling magmatic belt in the North China Craton: Implications for Paleoproterozoic tectonics. Lithos, 2012, 148: 27-44
[58]
53 Wan Y S, Wilde S A, Liu D Y, et al. Further evidence for ~1.85 Ga metamorphism in the central zone of the North China Craton: SHRIMP U-Pb dating of zircon from metamorphic rocks in the Lushan area, Henan Province. Gondwana Res, 2006, 9: 189-197
[59]
55 Jahn B M, Liu D Y, Wan Y S, et al. Archean crustal evolution of the Jiaodong Peninsula, China, as revealed by zircon SHRIMP geochronology, elemental and Nd-isotope geochemistry. Am J Sci, 2008, 308: 232-269
[60]
56 Wan Y S, Liu D Y, Wang S J, et al. ~2.7 Ga juvenile crust formation in the North China Craton (Taishan-Xintai area, western Shandong province): Further evidence of an understated event from U-Pb dating and Hf isotopic composition of zircon. Precambrian Res, 2011, 186: 169-180
[61]
58 Geng Y S, Du L L, Ren L D. Growth and reworking of the Early precambrian continental crust in the North China Craton: Constraints from zircon Hf isotopes. Gondwana Res, 2012, 21: 517-529
[62]
61 Valley J W. Oxygen isotopes in zircon. Rev Mineral Geochem, 2003, 53: 343-385
[63]
62 Kemp AIS, Hawkesworth C J, Paterson B A, et al. Episodic growth of the Gondwana supercontinent from Hafnium and Oxygen isotopes in zircon. Nature, 2006, 439: 580-583
[64]
64 Trap P, Faure M, Lin W, et al. Late Paleoproterozoic (1900-1800 Ma) nappe stacking and polyphase deformation in the Hengshan- Wutaishan area: Implications for the understanding of the Trans-North-China belt, North China Craton. Precambrian Res, 2007, 156: 85-106
[65]
65 Trap P, Faure M, Lin W, et al. Paleoproterozoic tectonic evolution of the Trans-North China Orogen: Toward a comprehensive model. Precambrian Res, 2012, 222-223: 191-211
67 Collins W J, Belousova E A, Kemp A, et al. Two contrasting Phanerozoic orogenic systems revealed by Hafnium isotope data. Nat Geosci, 2011, 4: 333-337
[68]
68 Gutscher M A, Dominguez S, Westbrook G K, et al. The gibraltar subduction: A decade of new geophysical data. Tectonophysics, 2012, 574-575: 72-91ib Mineral Petrol, 2005, 150: 561-580
[69]
61 Valley J W. Oxygen isotopes in zircon. Rev Mineral Geochem, 2003, 53: 343 -385
[70]
62 Kemp AIS, Hawkesworth C J, Paterson B A, et al. Episodic growth of the Gondwana supercontinent from Hafnium and Oxygen isotopes in zircon. Nature, 2006, 439: 580-583
64 Trap P, Faure M, Lin W, et al. Late Paleoproterozoic (1900-1800 Ma) nappe stacking and polyphase deformation in the Hengshan- Wutaishan area: Implications for the understanding of the Trans-North-China belt, North China Craton. Precambrian Res, 2007, 156:85-106
[73]
65 Trap P, Faure M, Lin W, et al. Paleoproterozoic tectonic evolution of the Trans-North China Orogen: Toward a comprehensive model. Precambrian Res, 2012, 222-223: 191-211
67 Collins W J, Belousova E A, Kemp A, et al. Two contrasting Phanerozoic orogenic systems revealed by Hafnium isotope data. Nat Geosci,2011, 4: 333-337
[76]
68 Gutscher M A, Dominguez S, Westbrook G K, et al. The gibraltar subduction: A decade of new geophysical data. Tectonophysics, 2012,574-575: 72-91 ?