[1] Chapple, W. M., 1978. Mechanics of Thin-Skinned Fold-and-Thrust Belts. Geological Society of American Bulletin, 89: 1189–1198 doi: 10.1130/0016-7606(1978)89<1189:MOTFB>2.0.CO;2
[2] Chen, Y. L., Luo, Z. H., Liu, C., 2001. New Recognition of Kangding-Mianning Metamorphic Complexes from Sichuan, Western Yangtze Craton: Evidence from Nd Isotopic Compositon. Earth Science-Journal of China University of Geosciences, 26(3): 279–285 (in Chinese with English Abstract)
[3] Condie, K. C., Belousova, E., Griffin, W. L., et al., 2009. Granitoid Events in Space and Time: Constraints from Igneous and Detrital Zircon Age Spectra. Gondwana Research, 15: 228–242 doi: 10.1016/j.gr.2008.06.001
[4] Davis, D., Suppe, J., Dahlen, F. A., 1983. Mechanics of Fold-and-Thrust Belts and Accretionary Wedges. Journal of Geophysical Research, 88(B2): 1153–1172, doi: 10.1029/JB088iB02p01153
[5] Feng, D. Y., Li, Z. C., Zhang, Z. C., 1991. Intrusive Ages and Isotopic Characteristics of Massives in the South of Huangling Granitoids. Hubei Geology, 5(2): 1–12 (in Chinese with English Abstract)
[6] Fu, G. Q., Yuan, H. H., Li, S. L., 1993. Discovery of Archean Granite-Greenstone Terrain of the Northern Huangling Block, Western Hubei Province, China. J. Mineral. Petrol. , 13(1): 5–13 (in Chinese with English Abstract)
[7] Gao, S., Ling, W. L., Qiu, Y., et al., 1999. Contrasting Geochemical and Sm-Nd Isotopic Compositions of Archean Metasediments from the Kongling High-Grade Terrain of the Yangtze Craton: Evidence for Cratonic Evolution and Redistribution of REE during Crustal Anatexis. Geochimica et Cosmochimica Acta, 63(13–14): 2071–2088
[8] Gao, S., Qiu, Y. M., Ling, W. L., et al., 2001. The Single Grain Zircon SHRIMP U-Pb Geochronology from Kongling High-Grade Metamorphic Terrain-Discovery of > 3.2 Ga Continental Crust in Yangtze Craton. Science in China (Series D), 31(1): 27–35 (in Chinese)
[9] Golonka, J., 2004. Plate Tectonic Evolution of the Southern Margin of Eurasia in the Mesozoic and Cenozoic. Tectonophysics, 381(1–4): 235–273 http://www.geo.edu.ro/sgr/mod/downloads/PDF/Golonka-TPh-2004.pdf
[10] Hans, L., 2010. Jura, Alps and the Boundary of the Adria Subplate. Tectonophysics, 484(1–4): 223–239 http://www.onacademic.com/detail/journal_1000035440838910_5399.html
[11] Hinton, R. W., Upton, B. G. J., 1991. The Chemistry of Zircon: Variations within and between Large Crystals from Syenite and Alkali Basalt Xenoliths. Geoehimica et Cosmoehimica Acta, 55(11): 3287–3302 doi: 10.1016/0016-7037(91)90489-R
[12] Hoskin, P. W. O., Ireland, T. I., 2000. Rare Earth Element Chemistry of Zircon and Its Use as a Provenance Indicator. Geology, 28(7): 627–630 doi: 10.1130/0091-7613(2000)28<627:REECOZ>2.0.CO;2
[13] Jiang, J. S., 1986. Isotopic Geochronology and Crustal Evolution of Huangling Metamorphic Terrain. Journal of Changchun College of Geology, 3: 1–11 (in Chinese with English Abstract)
[14] Li, X. H., Liang, X. R., Sun, M., et al., 2000. Geochronology and Geochemistry of Single-Grain Zircons: Simultaneous In-Situ Analysis of U-Pb Age and Trace Elements by LAM-ICP-MS. Eur. J. Mineral. , 12: 1015–1024, doi: 10.1127/0935-1221/2000/0012-1015
[15] Li, X. H., Wang, X. C., Li, W. X., et al., 2008. Petrogenesis and Tectonic Significance of Neoproterozoic Basaltic Rocks in South China: From Orogenesis to Intracontinental Rifting. Geochimica, 37(4): 382–398 (in Chinese with English Abstract) http://www.zhangqiaokeyan.com/academic-journal-cn_geochimica_thesis/0201252980354.html
[16] Li, Y. L., Zhou, H. W., Li, X. H., et al., 2007. 40Ar-39Ar Plateau Ages of Biotite and Amphibole from Tonalite of Huangling Granitoids and Their Cooling Curve. Acta Petrologica Sinica, 23(5): 1067–1074 (in Chinese with English Abstract)
[17] Li, Z. C., Wang, G. H., Zhang, Z. C., 2002. Isotopic Age Spectrum of the Huangling Granitic Batholith, Western Hubei. Geology and Mineral Resources of South China, 3: 19–28 (in Chinese with English Abstract)
[18] Li, Z. X., Li, X. H., Kinny, P. D., et al., 2003. Geochronology of Neoproterozoic Syn-Rift Magmatism in the Yangtze Craton, South China and Correlations with Other Continents: Evidence for a Mantle Superplume that Broke-Up Rodinia. Precambrian Research, 122(1–4): 85–109
[19] Ling, W. L., Gao, S., Zhang, B. R., et al., 2000. Late Paleoproterozoic Tectonic Thermal Event within the Yangtze Continental Interior and Its Evolution. Chinese Science Bulletin, 45(21): 2343–2348 (in Chinese) doi: 10.1360/csb2000-45-21-2343
[20] Ling, W. L., Gao, S., Zhang, B. R., et al., 2003. Neoproterozoic Tectonic Evolution of the Northwestern Yangtze Craton, South China: Implications for Amalgamation and Breakup of the Rodinia Supercontinent. Precambrian Research, 122(1–4): 111–140 http://www.sciencedirect.com/science/article/pii/S030192680200222X
[21] Liu, Y. S., Hu, Z. C., Gao, S., et al., 2008. In Situ Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS without Applying an Internal Standard. Chemical Geology, 257(1–2): 34–43 http://cms.kdis.edu.cn/cms/geology_cug/achievements/fabiaowenzhang/resource/414f3b8022107c51b3554fd7277929d6.pdf
[22] Liu, Y. S., Gao, S., Hu, Z. C., et al., 2010a. Continental and Oceanic Crust Recycling-Induced Melt-Peridotite Interactions in the Trans-North China Orogen: U-Pb Dating, Hf Isotopes and Trace Elements in Zircons of Mantle Xenoliths. Journal of Petrology, 51(1–2): 537–571, doi: 10.1093/petrology/egp082
[23] Liu, Y. S., Hu, Z. C., Zong, K. Q., et al., 2010b. Reappraisement and Refinement of Zircon U-Pb Isotope and Trace Element Analyses by LA-ICP-MS. Chinese Science Bulletin, 55(15): 1535–1546, doi: 10.1007/s11434-010-3052-4
[24] Ludwig, K. R., 2003. ISOPLOT 3.00: A Geochronological Toolkit for Microsoft Excel. Berkeley Geochronology Center, Berkeley
[25] Ma, D. Q., Du, S. H., Xiao, Z. F., 2002. The Origin of Huangling Granite Batholith. Acta Petrologica et Mineralogica, 21(2): 151–161 (in Chinese with English Abstract)
[26] Peng, M., Wu, Y. B., Wang, J., et al., 2009. Paleoproterozoic Mafic Dyke from Kongling Terrain in the Yangtze Craton and Its Implication. Chinese Science Bulletin, 54(5): 641–647, doi:10.1007/s11434-008-0558-0 (in Chinese)
[27] Peng, S. B., Li, C. N., Kusky, T. M., et al., 2010. Discovery and Its Tectonic Significance of the Proterozoic Miaowan Ophiolites in the Southern Huangling Anticline, Western Hubei, China. Geological Bulletin of China, 29(1): 8–20 (in Chinese with English Abstract)
[28] Peng, S. B., Kusky, T. M., Jiang, X. F., et al., 2012. Geology, Geochemistry, and Geochronology of the Miaowan Ophiolite, Yangtze Craton: Implications for South China's Amalgamation History with the Rodinian Supercontinent. Gondwana Research, 21(2-3): 577–594, doi: 10.1016/j.gr.2011.07.010
[29] Peresson, H., Decker, K., 1997. The Tertiary Dynamics of the Northern Eastern Alps (Austria): Changing Palaeostresses in a Collisional Plate Boundary. Tectonophysics, 272(2–4): 125–157 http://adsabs.harvard.edu/abs/1997Tectp.272..125P
[30] Qiu, Y. M., Gao, S., Mcnaughton, N. J., et al., 2000. First Evidence of > 3.2 Ga Continental Crust in the Yangtze Craton of South China and Its Implications for Archean Crustal Evolution and Phanerozoic Tectonics. Geology, 28(1): 11–14, doi:10.1130/0091-7613(2000)028<0011:FEOGCC>2.0.CO;2
[31] Rodgers, J., 1990. Fold-and-Thrust Belts in Sedimentary, Part Ⅰ: Typical Examples. American Journal of Science, 290: 321–359, doi: 10.2475/ajs.290.4.321
[32] Rodgers, J., 1991. Fold-and-Thrust Belts in Sedimentary, Part Ⅱ: Other Examples, Especially Variants. American Journal of Science, 291: 825–886, doi: 10.2475/ajs.291.9.825
[33] Samson, S. D., Coler, D. G., Speer, J. A., 1995. Geochemical and Nd-Sr-Pb Isotopic Composition of Alleghanian Granites of the Southern Appalachians: Origin, Tectonic Setting, and Source Characterization. Earth and Planetary Science Letters, 134(3–4): 359–376 http://www.sciencedirect.com/science/article/pii/0012821X9500124U
[34] Sasseville, C., Tremblay, A., Clauer, N., et al., 2008. K-Ar Age Constraints on the Evolution of Polydeformed Fold-Thrust Belts: The Case of the Northern Appalachians (Southern Quebec). Journal of Geodynamics, 45(2–3): 99–119, doi: 10.1016/j.jog.2007.07.004
[35] Simony, P. S., Carr, S. D., 2011. Cretaceous to Eocene Evolution of the Southeastern Canadian Cordillera: Continuity of Rocky Mountain Thrust Systems with Zones of "In-Sequence" Mid-Crustal Flow. Journal of Structural Geology, 33(9): 1417–1434 doi: 10.1016/j.jsg.2011.06.001
[36] Song, C. Z., Liu, G. S., Niu, M. L., et al., 2002. Cenozoic Structures and Dynamics on the Northern Margin of Qinling-Dabie Orogenic Belt. Geological Bulletin of China, 21(8–9): 530–535 (in Chinese with English Abstract) http://www.zhangqiaokeyan.com/academic-journal-cn_geological-bulletin-china_thesis/0201252294480.html
[37] Sun, S. S., McDonough, W. F., 1989. Chemical and Isotopic Systematics of Oceanic Basalts: Implications for Mantle Composition and Processes. In: Saunders, A. D., Norry, M. J., eds., Magmatism of the Ocean Basins. Geological Society, London, Special Publications, 42: 313–345, doi: 10.1144/GSL.SP.1989.042.01.19
[38] Sun, X. M., Wu, G. Y., Hao, F. J., et al., 2004. Epochs and Space-Time Migrating of Meso-Cenozoic Thrust-Nappe Tectonics in the North Qinling-Dabie Orogen. Chinese Journal of Geology, 39(1): 63–76 (in Chinese with English Abstract)
[39] Thakur, V. C., 1980. Tectonics of the Central Crystallines of Western Himalaya. Tectonophysics, 62(1–2): 141–154
[40] Tremblay, A., Ruffet, G., Bédard, J. H., 2011. Obduction of Tethyan-Type Ophiolites-A Case-Study from the Thetford-Mines Ophiolitic Complex, Quebec Appalachians, Canada. Lithos, 125(1-2): 10–26 doi: 10.1016/j.lithos.2011.01.003
[41] Wang, X. F., Ma, D. Q., Chen, X. H., et al., 2001. Precambrian Evolution of the Huangling Arch, China and Its Relation to the Rodinia Breakup and Assembly. Gondwana Research, 4(4): 816–817 doi: 10.1016/S1342-937X(05)70603-1
[42] Wang, J., Liu, B. J., Pan, G. T., 2001. Neoproterozoic Rifting History of South China Significance to Rodinia Breakup. J. Mineral. Petrol., 21(3): 135–145 (in Chinese with English Abstract) http://www.cnki.com.cn/Article/CJFDTotal-KWYS200103020.htm
[43] Wei, Y. X., Peng, S. B., Jiang, X. F., et al., 2012. SHRIMP Zircon U-Pb Ages and Geochemical Characteristics of the Neoproterozoic Granitoids in the Huangling Anticline and Its Tectonic Setting. Journal of Earth Science, 23(5): 659–675 doi: 10.1007/s12583-012-0284-z
[44] Wiedenbeck, M., Alle, P., Corfu, F., et al., 1995. Three Natural Zircon Standards for U-Th-Pb, Lu-Hf, Trace Element and REE Analyses. Geostandards and Geoanalytical Research, 19(1): 1–23, doi: 10.1111/j.1751-908X.1995.tb00147.x
[45] Wu, Y. B., Chen, D. G., Xia, Q. K., et al., 2002. Trace Element Analysis of Zircons from Eclogite in Huangzhen in Dabie: Trace Element Characteristics of Eclogite-Facies Metamorphic Zircons. Chinese Science Bulletin, 47(11): 859–863 (in Chinese) doi: 10.1360/csb2002-47-11-859
[46] Wu, Y. B., Chen, D. G., Xia, Q. K., et al., 2003. Granulite in the Dabie Mountains Huangtuling Zircon LAM-ICP-MS Trace Element Analysis and Pb-Pb Dating. Science in China (Series D), 33(1): 20–28 (in Chinese)
[47] Xie, D. N., He, M. X., Zhou, L. F., et al., 2006. Characteristics of Overthrust Structures on Northern Edge of East Qinling-Dabie Orogenic Belt and Hydrocarbon Potentials. Oil & Gas Geology, 27(1): 48–55 (in Chinese with English Abstract) http://ogg.pepris.com/EN/Y2006/V27/I1/48
[48] Xiong, Q., Zheng, J. P., Yu, C. M., et al., 2008. Zircon U-Pb Age and Hf Isotope of Quanyishang A-Type Granite in Yichang: Signification for the Yangtze Continental Cratonization in Paleoproterozoic. Chinese Science Bulletin, 53(22): 2782–2792 (in Chinese) doi: 10.1360/csb2008-53-22-2782
[49] Ye, P. S., 2004. Ophiolites and Thrust System of Middle Lhasa Block: [Dissertation]. Chinese Academy of Geological Sciences, Beijing. 16–17 (in Chinese with English Abstract)
[50] Zhang, C. H., Song, H. L., 1997. Mesozoic Thrust Tectonic in Yanshan Intraplate Orogen and the Differences between Them and Those of Foreland Fold-and-Thrust Belt. Earth Science-Journal of China University of Geosciences, 22(1): 33–36 (in Chinese with English Abstract)
[51] Zhang, S. B., Zheng, Y. F., Wu, Y. B., et al., 2006. Zircon U-Pb Age and Hf-O Isotope Evidence for Paleoproterozoic Metamorphic Event in South China. Precambrian Research, 151(3–4): 265–288
[52] Zhang, S. B., Zheng, Y. F., Zhao, Z. F., et al., 2009. Origin of TTG-Like Rocks from Anatexis of Ancient Lower Crust: Geochemical Evidence from Neoproterozoic Granitoids in South China. Lithos, 113: 347–368, doi: 10.1016/j.lithos.2009.04.024
[53] Zhang, S. B., Zheng, Y. F., Zhao, Z. F., 2010. Temperature Effect over Garnet Effect on Uptake of Trace Elements in Zircon of TTG-Like Rocks. Chemical Geology, 274: 108–125, doi: 10.1016/j.chemgeo.2010.04.002
[54] Zhao, J. H., Zhou, M. F., Zheng, J. P., 2010. Metasomatic Mantle Source and Crustal Contamination for the Formation of the Neoproterozoic Mafic Dike Swarm in the Northern Yangtze Block, South China. Lithos, 115: 177–189, doi: 10.1016/j.lithos.2009.12.001
[55] Zheng, Y. F., Zhang, S. B., 2007. Formation and Evolution of the Precambrian Continental Crust in South China. Chinese Science Bulletin, 52(1): 1–10 (in Chinese) doi: 10.1007/s11434-007-0015-5
[56] Zhou, Z. Y., Yang, J. X., Zhou, H. W., et al., 2007. Significance on Hubei Huangling Complex in the Rodinia Supercontinent of Evolution. Resources Environment and Engineering, 21(4): 380–384 (in Chinese with English Abstract)