Hostname: page-component-7c8c6479df-fqc5m Total loading time: 0 Render date: 2024-03-28T09:21:08.572Z Has data issue: false hasContentIssue false

Petrogenesis of Silurian ultramafic–mafic plutons in southern Jiangxi: implications for the Wuyi–Yunkai orogen, South China

Published online by Cambridge University Press:  04 December 2020

Jie Yang
Affiliation:
Shandong Provincial Key Laboratory of Depositional Mineralization and Sedimentary Minerals, College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao266590, PR China
Wei Liu*
Affiliation:
Institute of Surface-Earth System Science, Tianjin University, Tianjin300072, PR China
Zuozhen Han*
Affiliation:
Shandong Provincial Key Laboratory of Depositional Mineralization and Sedimentary Minerals, College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao266590, PR China Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao266237, PR China
Zuoxun Zeng
Affiliation:
School of Earth Sciences, China University of Geosciences, Wuhan430074, PR China
Le Wan
Affiliation:
School of Earth Sciences, China University of Geosciences, Wuhan430074, PR China
Adil S. Mohammed
Affiliation:
School of Earth Sciences, China University of Geosciences, Wuhan430074, PR China
*
Authors for correspondence: Wei Liu, Email: weiliutu@163.com; Zuozhen Han, Email: hanzuozhen65@126.com
Authors for correspondence: Wei Liu, Email: weiliutu@163.com; Zuozhen Han, Email: hanzuozhen65@126.com

Abstract

The South China Block is one of the largest continental blocks located on the East Asian continent. The early Palaeozoic Wuyi–Yunkai orogen of the South China Block (known as the Caledonian orogen in Europe) is a major orogenic belt in East Asia and represents the first episode of extensive crustal reworking since Neoproterozoic time. Although this orogen is key to deciphering the formation and evolution of the South China Block, details about the orogen remain poorly defined. The Songshutang and Wushitou ultramafic–mafic units in southern Jiangxi Province, South China, have 206Pb–238U ages of c. 437 Ma, suggesting a Silurian formation age. All the Songshutang and Wushitou ultramafic–mafic rocks show relatively flat chondrite-normalized rare earth element patterns, depletions in Nb, Ta, Zr, Hf and Ti, and low ϵNd(t) values from −9.12 to −5.49 with negative zircon ϵHf(t) values from −10.84 to −2.58, resembling a typical arc magma affinity. Geochemical and isotopic data indicate that the newly identified ultramafic–mafic rocks, along with the reported Silurian mafic rocks in South China, possibly originated from the similar partial melting of an ancient subducted slab, fluid/sediment and metasomatized lithospheric mantle with varying degrees of fractional crystallization. In conjunction with other records of magmatism and metamorphism in South China, a late-orogenic extensional event led to the melting of the sub-continental lithospheric mantle in Silurian time and generated ultramafic–mafic rocks with a limited distribution along the Wuyi–Yunkai orogen and widespread late-orogenic granitic plutons in the South China Block.

Type
Original Article
Copyright
© The Author(s), 2020. Published by Cambridge University Press

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Baker, JA, Menzies, MA, Thirlwall, MF and Macpherson, CG (1997) Petrogenesis of Quaternary intraplate volcanism, Sana’a, Yemen: implications for plume–lithosphere interaction and polybaric melt hybridization. Journal of Petrology 38, 1359–90.CrossRefGoogle Scholar
Campbell, IH and Griffiths, RW (1993) The evolution of the mantle’s chemical structure. Lithos 30, 389–99.CrossRefGoogle Scholar
Carter, A, Roques, D, Bristow, C and Kinny, P (2001) Understanding Mesozoic accretion in Southeast Asia: significance of Triassic thermotectonism (Indosinian orogeny) in Vietnam. Geology 29, 211–14.2.0.CO;2>CrossRefGoogle Scholar
Cawood, PA, Wang, Y, Xu, Y and Zhao, G (2013) Locating South China in Rodinia and Gondwana: a fragment of greater India lithosphere? Geology 41, 903–6.CrossRefGoogle Scholar
Charvet, J (2013) The Neoproterozoic–Early Paleozoic tectonic evolution of the South China Block: an overview. Journal of Asian Earth Sciences 74, 198209.CrossRefGoogle Scholar
Charvet, J, Shu, L, Faure, M, Choulet, F, Wang, B, Lu, H and Le Breton, N (2010) Structural development of the Lower Paleozoic belt of South China: genesis of an intracontinental orogen. Journal of Asian Earth Sciences 39, 309–30.CrossRefGoogle Scholar
Chen, X, Tong, L, Zhang, C, Zhu, Q and Li, Y (2015) Retrograde garnet amphibolite from eclogite of the Zhejiang Longyou area: new evidence of the Caledonian orogenic event in the Cathaysia block. Chinese Science Bulletin 60, 1207–17.Google Scholar
Cox, KG (1980) A model for flood basalt vulcanism. Journal of Petrology 21, 629–50.CrossRefGoogle Scholar
Cui, X, Jiang, X, Wang, J, Wang, X, Zhuo, J, Deng, Q, Liao, S, Wu, H, Jiang, Z and Wei, Y (2015) Mid-Neoproterozoic diabase dykes from Xide in the western Yangtze Block, South China: new evidence for continental rifting related to the breakup of Rodinia supercontinent. Precambrian Research 268, 339–56.CrossRefGoogle Scholar
DePaolo, DJ (1981) Trace element and isotopic effects of combined wallrock assimilation and fractional crystallization. Earth and Planetary Science Letters 53, 189202.CrossRefGoogle Scholar
Depaolo, DJ and Daley, EE (2000) Neodymium isotopes in basalts of the southwest basin and range and lithospheric thinning during continental extension. Chemical Geology 169, 157–85.CrossRefGoogle Scholar
Falloon, TJ, Green, DH, Hatton, C and Harris, K (1988) Anhydrous partial melting of a fertile and depleted peridotite from 2 to 30 kb and application to basalt petrogenesis. Journal of Petrology 29, 1257–82.CrossRefGoogle Scholar
Faure, M, Shu, L, Wang, B, Charvet, J, Choulet, F and Monié, P (2009) Intracontinental subduction: a possible mechanism for the Early Palaeozoic orogen of SE China. Terra Nova 21, 360–8.CrossRefGoogle Scholar
Feng, SJ, Zhao, KD, Ling, HF, Chen, PR, Chen, WF, Sun, T, Jiang, SY and Pu, W (2014) Geochronology, elemental and Nd–Hf isotopic geochemistry of Devonian A-type granites in central Jiangxi, South China: constraints on petrogenesis and post-collisional extension of the Wuyi–Yunkai orogeny. Lithos 206–207, 118.CrossRefGoogle Scholar
Furman, T and Graham, D (1999) Erosion of lithospheric mantle beneath the East African Rift system: geochemical evidence from the Kivu volcanic province. In Composition, Deep Structure and Evolution of Continents (eds van der Hilst, RD and McDonough, WF), pp. 237–62. Developments in Geotectonics vol. 24. Amsterdam: Elsevier.CrossRefGoogle Scholar
Garcia, MO, Foss, DJP, West, HB and Mahoney, JJ (1996) Geochemical and isotopic evolution of Loihi Volcano, Hawaii. Journal of Petrology 37, 1647–74.CrossRefGoogle Scholar
Hastie, AR, Mitchell, SF, Treloar, PJ, Kerr, AC, Neill, I and Barfod, DN (2013) Geochemical components in a Cretaceous island arc: the Th/La–(Ce/Ce*) Nd diagram and implications for subduction initiation in the inter-American region. Lithos 162, 5769.CrossRefGoogle Scholar
He, WH, Tang, TT, Yue, ML, Deng, JF, Pan, GT, Xing, GF, Luo, MS, Xu, YD, Wei, Y, Zhang, ZY, Xiao, YF and Zhang, KX (2014) Sedimentary and tectonic evolution of Nanhuan–Permian in South China. Earth Science (Journal of China University of Geosciences) 39, 929–53 (in Chinese with English abstract).Google Scholar
Herzberg, C and Asimow, PD (2015) PRIMELT3 MEGA.XLSM software for primary magma calculation: peridotite primary magma MgO contents from the liquidus to the solidus. Geochemistry, Geophysics, Geosystems 16, 563–78.CrossRefGoogle Scholar
Hole, MJ, Saunders, AD, Marriner, GF and Tarney, J (1984) Subduction of pelagic sediments: implications for the origin of Ce-anomalous basalts from the Mariana Islands. Journal of the Geological Society, London 141, 453–72.CrossRefGoogle Scholar
Hoskin, PWO and Ireland, TR (2000) Rare earth element chemistry of zircon and its use as a provenance indicator. Geology 28, 627–30.2.0.CO;2>CrossRefGoogle Scholar
Hoskin, PWO and Schaltegger, U (2003) The composition of zircon and igneous and metamorphic petrogenesis. Reviews in Mineralogy and Geochemistry 53, 2762.CrossRefGoogle Scholar
Hu, L, Cawood, PA, Du, Y, Xu, Y, Wang, C, Wang, Z, Ma, Q and Xu, X (2017) Permo-Triassic detrital records of South China and implications for the Indosinian events in East Asia. Palaeogeography, Palaeoclimatology, Palaeoecology 485, 84100.CrossRefGoogle Scholar
Hu, L, Du, Y, Cawood, PA, Xu, Y, Yu, W, Zhu, Y and Yang, J (2014) Drivers for late Paleozoic to early Mesozoic orogenesis in South China: constraints from the sedimentary record. Tectonophysics 618, 107–20.CrossRefGoogle Scholar
Hu, Z, Gao, S, Liu, Y, Hu, S, Chen, H and Yuan, H (2008) Signal enhancement in laser ablation ICP-MS by addition of nitrogen in the central channel gas. Journal of Analytical Atomic Spectrometry 23, 1093–101.CrossRefGoogle Scholar
Hu, Z, Liu, Y, Gao, S, Liu, W, Zhang, W, Tong, X, Lin, L, Zong, K, Li, M and Chen, H (2012) Improved in situ Hf isotope ratio analysis of zircon using newly designed X skimmer cone and jet sample cone in combination with the addition of nitrogen by laser ablation multiple collector ICP-MS. Journal of Analytical Atomic Spectrometry 27, 1391–9.CrossRefGoogle Scholar
Hu, PY, Zhai, QG, Ren, GM, Wang, J and Tang, Y (2018) Late Ordovician high-Mg adakitic andesite in the western South China block: evidence of oceanic subduction. International Geology Review 60, 1140–54.CrossRefGoogle Scholar
Huang, T (1980) An outline of the tectonic characteristics of China. Continental Tectonics 36, 184–97.Google Scholar
Huang, D and Wang, X (2019) Reviews of geochronology, geochemistry, and geodynamic processes of Ordovician–Devonian granitic rocks in southeast China. Journal of Asian Earth Sciences 184, 104001. doi: 10.1016/j.jseaes.2019.104001.CrossRefGoogle Scholar
Jia, XH, Wang, XD and Yang, WQ (2017) Petrogenesis and geodynamic implications of the early Paleozoic potassic and ultrapotassic rocks in the South China Block. Journal of Asian Earth Sciences 135, 8094.CrossRefGoogle Scholar
Kessel, R, Schmidt, MW, Ulmer, P and Pettke, T (2005) Trace element signature of subduction-zone fluids, melts and supercritical liquids at 120–180 km depth. Nature 437, 724.CrossRefGoogle ScholarPubMed
Kim, SW, Oh, CW, Williams, IS, Rubatto, D, Ryu, IC, Rajesh, V, Kim, CB, Guo, J and Zhai, M (2006) Phanerozoic high-pressure eclogite and intermediate-pressure granulite facies metamorphism in the Gyeonggi Massif, South Korea: implications for the eastward extension of the Dabie–Sulu continental collision zone. Lithos 92, 357–77.CrossRefGoogle Scholar
Langmuir, CH, Klein, EM and Plank, T (1992) Petrological systematics of mid-ocean ridge basalts: constraints on melt generation beneath ocean ridges. In Mantle Flow and Melt Generation at Mid-Ocean Ridges (eds Phipps Morgan, J, Blackman, DK and Sinton, JM), pp. 183280. American Geophysical Union, Geophysical Monograph vol. 71. Washington, DC, USA.Google Scholar
Li, HB, Jia, D, Wu, L, Zhang, Y, Yin, HW, Wei, GQ and Li, BL (2013) Detrital zircon provenance of the Lower Yangtze foreland basin deposits: constraints on the evolution of the early Palaeozoic Wuyi–Yunkai orogenic belt in South China. Geological Magazine 150, 959–74.CrossRefGoogle Scholar
Li, ZX and Li, XH (2007) Formation of the 1300-km-wide intracontinental orogen and postorogenic magmatic province in Mesozoic South China: a flat-slab subduction model. Geology 35, 179–82.CrossRefGoogle Scholar
Li, ZX, Li, X, Wartho, JA, Clark, C, Li, W, Zhang, CL and Bao, C (2010) Magmatic and metamorphic events during the Early Paleozoic Wuyi–Yunkai orogeny, southeastern South China; new age constraints and pressure–temperature conditions. Geological Society of America Bulletin 122, 772–93.CrossRefGoogle Scholar
Li, X, Li, Z, Zhou, H, Liu, Y and Kinny, PD (2002) U–Pb zircon geochronology, geochemistry and Nd isotopic study of Neoproterozoic bimodal volcanic rocks in the Kangdian Rift of South China: implications for the initial rifting of Rodinia. Precambrian Research 113, 135–54.CrossRefGoogle Scholar
Li, L, Lin, S, Li, J, He, J and Ge, Y (2017) Zircon U–Pb ages and Hf isotope compositions of the Chencai migmatite, central Zhejiang Province, South China: constraints on the early Palaeozoic orogeny. Geological Magazine 155, 1377–93.CrossRefGoogle Scholar
Lin, SF, Xing, GF, Davis, DW, Yin, CQ, Wu, ML, Li, LM, Jiang, Y and Chen, ZH (2018) Appalachian-style multi-terrane Wilson cycle model for the assembly of South China. Geology 46, 319–22.CrossRefGoogle Scholar
Liu, S, Peng, S, Kusky, T, Polat, A and Han, Q (2018) Origin and tectonic implications of an Early Paleozoic (460–440 Ma) subduction-accretion shear zone in the northwestern Yunkai Domain, South China. Lithos 322, 104–28.CrossRefGoogle Scholar
Liu, X, Wang, Q, Ma, L, Yang, JH, Guo, GN, Ou, Q and Wang, J (2020) Early Paleozoic intracontinental granites in the Guangzhou region of South China: partial melting of a metasediment-dominated crustal source. Lithos 376–377, 105763. doi: 10.1016/j.lithos.2020.105763.CrossRefGoogle Scholar
Ma, Q, Zheng, J, Griffin, WL, Zhang, M, Tang, H, Su, Y and Ping, X (2012) Triassic “adakitic” rocks in an extensional setting (North China): melts from the cratonic lower crust. Lithos 149, 159–73.CrossRefGoogle Scholar
Macdonald, R, Rogers, NW, Fitton, JG, Black, S and Smith, M (2001) Plume–lithosphere interactions in the generation of the basalts of the Kenya Rift, East Africa. Journal of Petrology 42, 877900.CrossRefGoogle Scholar
McKenzie, D and Bickle, MJ (1988) The volume and composition of melt generated by extension of the lithosphere. Journal of Petrology 29, 625–79.CrossRefGoogle Scholar
Naumann, TR and Geist, DJ (1999) Generation of alkalic basalt by crystal fractionation of tholeiitic magma. Geology 27, 423–6.2.3.CO;2>CrossRefGoogle Scholar
Nelson, DR (1992) Isotopic characteristics of potassic rocks: evidence for the involvement of subducted sediments in magma genesis. Lithos 28, 403–20.CrossRefGoogle Scholar
Ou, Q, Lai, JQ, Carvalho, BB, Zi, F, Kong, H, Li, B and Jiang, ZQ (2018) Different response to middle-Palaeozoic magmatism during intracontinental orogenic processes: evidence from southeastern South China Block. International Geology Review 61, 1504–21.CrossRefGoogle Scholar
Patchett, PJ, Kouvo, O, Hedge, CE and Tatsumoto, M (1982) Evolution of continental crust and mantle heterogeneity: evidence from Hf isotopes. Contributions to Mineralogy and Petrology 78, 279–97.CrossRefGoogle Scholar
Pearce, JA and Peate, DW (1995) Tectonic implications of the composition of volcanic arc magmas. Annual Review of Earth and Planetary Sciences 23, 251–85.CrossRefGoogle Scholar
Peng, TP, Fan, WM, Zhao, GC, Peng, BX, Xia, XP and Mao, YS (2015) Petrogenesis of the early Paleozoic strongly peraluminous granites in the Western South China Block and its tectonic implications. Journal of Asian Earth Sciences 98, 399420.CrossRefGoogle Scholar
Peng, SB, Jin, ZM, Fu, JM, Liu, YH, He, LQ and Cai, MH (2006) Geochemical characteristics of basic intrusive rocks in the Yunkai uplift, Guangdong-Guangxi, China, and their tectonic significance. Geological Bulletin of China 25, 434–41 (in Chinese with English abstract).Google Scholar
Peng, SB, Liu, SF, Lin, MS, Wu, CF and Han, QS (2016) Early Paleozoic subduction in Cathaysia (II): new evidence from the Dashuang high magnesian-magnesian andesite. Earth Science 41, 931–47 (in Chinese with English abstract).Google Scholar
Qiu, XF, Zhao, XM, Yang, HM, Lu, SS, Jiang, T and Wu, NW (2018) Petrogenesis of the Early Palaeozoic granitoids from the Yunkai massif, South China block: implications for a tectonic transition from compression to extension during the Caledonian orogenic event. Geological Magazine 155, 1776–92.CrossRefGoogle Scholar
Ren, J (1991). On the geotectonics of southern China. Acta Geologica Sinica (English Edition) 4, 111–30.Google Scholar
Scherer, EE, Cameron, KL and Blichert, TJ (2000) Lu–Hf garnet geochronology: closure temperature relative to the Sm–Nd system and the effects of trace mineral inclusions. Geochimica et Cosmochimica Acta 64, 3413–32.CrossRefGoogle Scholar
Shan, G, Rudnick, RL, Hong, LY, Xiao, ML, Yong, SL, Wen, LX, Wen, LL, John, A, Xuan, CW and Qing, HW (2004) Recycling lower continental crust in the North China craton. Nature 432, 892–7.Google Scholar
Sharma, M (1997) Siberian traps. In Large Igneous Provinces: Continental, Oceanic and Planetary Flood Volcanism (eds Mahoney, JJ and Coffin, MF), pp. 273–95. American Geophysical Union, Geophysical Monograph vol. 100. Washington, DC, USA.Google Scholar
Shu, L, Wang, B, Cawood, PA, Santosh, M and Xu, Z (2015) Early Paleozoic and Early Mesozoic intraplate tectonic and magmatic events in the Cathaysia Block, South China. Tectonics 34, 1600–21.CrossRefGoogle Scholar
Sklyarov, EV, Gladkochub, D, Mazukabzov, A, Menshagin, YV, Watanabe, T and Pisarevsky, S (2003) Neoproterozoic mafic dike swarms of the Sharyzhalgai metamorphic massif, southern Siberian craton. Precambrian Research 122, 359–76.CrossRefGoogle Scholar
Song, MJ, Shu, LS, Santosh, M and Li, JY (2015) Late Early Paleozoic and Early Mesozoic intracontinental orogeny in the South China Craton: geochronological and geochemical evidence. Lithos 232, 360–74.CrossRefGoogle Scholar
Sun, SS and McDonough, WF (1989) Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. In Magmatism in the Ocean Basins (eds Saunders, AD and Norry, MJ), pp. 313–45. Geological Society of London, Special Publication no. 42. Google Scholar
Wang, Y, Fan, W, Zhang, G and Zhang, Y (2013a) Phanerozoic tectonics of the South China Block: key observations and controversies. Gondwana Research 23, 1273–305.CrossRefGoogle Scholar
Wang, Y, Fan, W, Zhao, G, Ji, S and Peng, T (2007) Zircon U–Pb geochronology of gneissic rocks in the Yunkai massif and its implications on the Caledonian event in the South China Block. Gondwana Research 12, 404–16.CrossRefGoogle Scholar
Wang, J and Li, ZX (2003) History of Neoproterozoic rift basins in South China: implications for Rodinia break-up. Precambrian Research 122, 141–58.CrossRefGoogle Scholar
Wang, Y, Li, G, Wang, Q, Santosh, M and Chen, J (2020) Early Paleozoic granitoids from South China: implications for understanding the Wuyi–Yunkai orogen. International Geology Review 62, 243–61.CrossRefGoogle Scholar
Wang, J, Shu, L and Yu, J (2017) From the Neoproterozoic mafic rock to the Silurian high-grade metamorphic rock: evidence from zircon U–Pb geochronological, bulk-rock geochemical and mineral EPMA studies of Longyou garnet amphibolite in SE China. Journal of Asian Earth Sciences 141, 723.CrossRefGoogle Scholar
Wang, Y, Zhang, A, Fan, W, Zhang, Y and Zhang, Y (2013b) Origin of paleosubduction-modified mantle for Silurian gabbro in the Cathaysia Block: geochronological and geochemical evidence. Lithos 160–161, 3754.CrossRefGoogle Scholar
Wilson, M (1989) Igneous Petrogenesis. London: Chapman and Hall.CrossRefGoogle Scholar
Wu, Y and Zheng, Y (2004) Genesis of zircon and its constraints on interpretation of U–Pb age. Science Bulletin 49, 1554–69.CrossRefGoogle Scholar
Xia, Y, Xu, X, Zou, H and Liu, L (2014) Early Paleozoic crust–mantle interaction and lithosphere delamination in South China Block: evidence from geochronology, geochemistry, and Sr–Nd–Hf isotopes of granites. Lithos 184–187, 416–35.CrossRefGoogle Scholar
Xie, Y, Ma, Y, Zhao, G, Xie, C, Han, Y, Li, J, Liu, Q, Yao, J, Zhang, Y and Lu, Y (2020) Origin of the Heping granodiorite pluton: implications for syn-convergent extension and asthenosphere upwelling accompanying the early Paleozoic orogeny in South China. Gondwana Research 85, 149–68.CrossRefGoogle Scholar
Xu, YJ, Cawood, PA and Du, YS (2016) Intraplate orogenesis in response to Gondwana assembly: Kwangsian Orogeny, South China. American Journal of Science 316, 329–62.CrossRefGoogle Scholar
Xu, Y, Cawood, PA, Du, Y, Huang, H and Wang, X (2014) Early Paleozoic orogenesis along Gondwana’s northern margin constrained by provenance data from South China. Tectonophysics 636, 4051.CrossRefGoogle Scholar
Xu, C, Wang, Y, Zhang, Y, Xu, W and Gan, C (2019) Geochronological and geochemical constraints of Chidong Silurian gabbroic pluton in Yunkai domain and its tectonic implications. Earth Science 44, 1202–15 (in Chinese with English abstract).Google Scholar
Xu, W and Xu, X (2017) An early Paleozoic monzonorite-granite suite in the South China block: implications for the intracontinental felsic magmatism. Mineralogy and Petrology 111, 709–28.CrossRefGoogle Scholar
Xu, W, Xu, X and Zeng, G (2017) Crustal contamination versus an enriched mantle source for intracontinental mafic rocks: insights from early Paleozoic mafic rocks of the South China Block. Lithos 286–287, 388–95.CrossRefGoogle Scholar
Yang, J, Lyons, TW, Zeng, Z, Odigie, K, Bates, S and Hu, L (2019a) Geochemical constraints on the origin of Neoproterozoic cap carbonate in the Helan Mountains, North China: implications for mid-late Ediacaran glaciation? Precambrian Research 331, 105361. doi: 10.1016/j.precamres.2019.105361.CrossRefGoogle Scholar
Yang, J, Zeng, Z, Cai, X, Li, Z, Li, T, Meng, F and He, W (2013) Carbon and oxygen isotopes analyses for the Sinian carbonates in the Helan Mountain, North China. Science Bulletin 58, 3943–55.CrossRefGoogle Scholar
Yang, J, Zhu, Q, Zeng, Z and Wan, L (2019b) Zircon U–Pb ages and Hf isotope compositions of the Neoproterozoic magmatic rocks in the Helan mountains, North China. Geological Magazine 156, 2104–12.CrossRefGoogle Scholar
Yao, WH and Li, ZX (2016) Tectonostratigraphic history of the Ediacaran–Silurian Nanhua foreland basin in South China. Tectonophysics 674, 3151.CrossRefGoogle Scholar
Yao, WH and Li, ZX (2019) Tectonostratigraphy and provenance analysis to define the edge and evolution of the eastern Wuyi–Yunkai orogen, South China. Geological Magazine 156, 8398.CrossRefGoogle Scholar
Yao, WH, Li, ZX, Li, WX, Wang, XC, Li, XH and Yang, JH (2012) Post-kinematic lithospheric delamination of the Wuyi–Yunkai orogen in South China: evidence from ca. 435 Ma high-Mg basalts. Lithos 154, 115–29.CrossRefGoogle Scholar
Yu, Y, Huang, XL, Sun, M and He, PL (2018) Petrogenesis of granitoids and associated xenoliths in the early Paleozoic Baoxu and Enping plutons, South China: implications for the evolution of the Wuyi–Yunkai intracontinental orogen. Journal of Asian Earth Sciences 156, 5974.CrossRefGoogle Scholar
Yu, P, Zhang, Y, Zhou, Y, Weinberg, RF, Zheng, Y and Yang, W (2019). Melt evolution of crustal anatexis recorded by the early Paleozoic Baiyunshan migmatite-granite suite in South China. Lithos 332–333, 8398.CrossRefGoogle Scholar
Yu, P, Zheng, Y, Zhou, Y, Chen, B, Niu, J and Yang, W (2018) Zircon U–Pb geochronology and geochemistry of the metabasite and gabbro: implications for the Neoproterozoic and Paleozoic tectonic settings of the Qinzhou bay–Hangzhou bay suture zone, South China. Geological Journal 53, 2219–39.CrossRefGoogle Scholar
Zegers, TE and van Keken, PE (2001) Middle Archean continent formation by crustal delamination. Geology 29, 1083–6.2.0.CO;2>CrossRefGoogle Scholar
Zeng, W, Zhang, L, Zhou, H, Zhong, Z, Xiang, H, Liu, R, Jin, S, , X and Li, C (2008) Caledonian reworking of Paleoproterozoic basement in the Cathaysia Block: constraints from zircon U–Pb dating, Hf isotopes and trace elements. Chinese Science Bulletin 53, 895904.Google Scholar
Zhang, Q, Jiang, YH, Wang, GC, Liu, Z, Ni, CY and Qing, L (2015) Origin of Silurian gabbros and I-type granites in central Fujian, SE China: implications for the evolution of the early Paleozoic orogen of South China. Lithos 216, 285–97.CrossRefGoogle Scholar
Zhang, J, Liu, W, Yakymchuk, C, Sa, R, Zeng, Z, Ding, R, Tang, G, Liu, H, Xu, Q and Wang, Y (2019) Partial melting and crustal deformation during the Early Paleozoic Wuyi–Yunkai Orogeny: insights from zircon U–Pb geochronology and structural analysis of the Fuhuling Migmatites in the Yunkai Region, South China. Minerals 9, 621.CrossRefGoogle Scholar
Zhang, CL, Santosh, M, Zhu, QB, Chen, XY and Huang, WC (2015) The Gondwana connection of South China: evidence from monazite and zircon geochronology in the Cathaysia Block. Gondwana Research 28, 1137–51.CrossRefGoogle Scholar
Zhang, XS, Xu, XS, Xia, Y and Liu, L (2017) Early Paleozoic intracontinental orogeny and post-orogenic extension in the South China Block: insights from volcanic rocks. Journal of Asian Earth Sciences 141, 2442.CrossRefGoogle Scholar
Zhang, J, Ye, T, Li, S, Yuan, G, Dai, C, Zhang, H and Ma, Y (2016) The provenance and tectonic setting of the Lower Devonian sandstone of the Danlin Formation in Southeast Yangtze Plate, with implications for the Wuyi–Yunkai orogeny in South China Block. Sedimentary Geology 346, 2534.CrossRefGoogle Scholar
Zhang, CL, Zhu, QB, Chen, XY and Ye, HM (2016) Ordovician arc-related mafic intrusions in South China: implications for plate subduction along the southeastern margin of South China in the Early Paleozoic. Journal of Geology 124, 743–67.CrossRefGoogle Scholar
Zhao, G and Cawood, PA (1999) Tectonothermal evolution of the Mayuan Assemblage in the Cathaysia Block; implications for Neoproterozoic collision-related assembly of the South China Craton. American Journal of Science 299, 309–39.CrossRefGoogle Scholar
Zhao, G and Cawood, PA (2012) Precambrian geology of China. Precambrian Research 222, 1354.CrossRefGoogle Scholar
Zhao, L, Cui, X, Zhai, M, Zhou, X and Liu, B (2019) Emplacement and metamorphism of the mafic rocks from the Chencai Terrane within the Cathaysia Block: implications for the Paleozoic orogenesis of the South China Block. Journal of Asian Earth Sciences 173, 1128.CrossRefGoogle Scholar
Zhao, JH and Zhou, MF (2007) Geochemistry of Neoproterozoic mafic intrusions in the Panzhihua district (Sichuan Province, SW China): implications for subduction-related metasomatism in the upper mantle. Precambrian Research 152, 2747.CrossRefGoogle Scholar
Zhong, Y, Ma, C, Liu, L, Zhao, J, Zheng, J, Nong, J and Zhang, Z (2014) Ordovician appinites in the Wugongshan Domain of the Cathaysia Block, South China: geochronological and geochemical evidence for intrusion into a local extensional zone within an intracontinental regime. Lithos 198, 202–16.CrossRefGoogle Scholar
Zhong, YF, Ma, CQ, Zhang, C, Wang, SM, She, ZB, Liu, L and Xu, HJ (2013) Zircon U–Pb age, Hf isotopic compositions and geochemistry of the Silurian Fengdingshan I-type granite pluton and Taoyuan mafic–felsic complex at the southeastern margin of the Yangtze Block. Journal of Asian Earth Sciences 74, 1124.CrossRefGoogle Scholar
Supplementary material: File

Yang et al. supplementary material

Tables S1-S5

Download Yang et al. supplementary material(File)
File 534.5 KB