Hostname: page-component-76fb5796d-r6qrq Total loading time: 0 Render date: 2024-04-27T19:43:10.361Z Has data issue: false hasContentIssue false
  • English
  • Français

Petrogenesis and tectonic implications of Late Mesoproterozoic A1- and A2-type felsic lavas from the Huili Group, southwestern Yangtze Block

Published online by Cambridge University Press:  08 January 2019

Dong-Bing Wang Open the ORCID record for Dong-Bing Wang [Opens in a new window] ,
Bao-Di Wang ,
Fu-Guang Yin ,
Zhi-Ming Sun ,
Shi-Yong Liao ,
Yuan Tang ,
Liang Luo  and
Zheng Liu
Dong-Bing Wang*
Affiliation:
Chengdu Centre, Chinese Geological Survey, Chengdu 610081, China
Bao-Di Wang
Affiliation:
Chengdu Centre, Chinese Geological Survey, Chengdu 610081, China
Fu-Guang Yin
Affiliation:
Chengdu Centre, Chinese Geological Survey, Chengdu 610081, China
Zhi-Ming Sun
Affiliation:
Chengdu Centre, Chinese Geological Survey, Chengdu 610081, China
Shi-Yong Liao
Affiliation:
Key Laboratory of Planetary Sciences, Purple Mountain Observatory, Chinese Academy of Sciences, Nanjing 210008, China
Yuan Tang
Affiliation:
Chengdu Centre, Chinese Geological Survey, Chengdu 610081, China
Liang Luo
Affiliation:
Chengdu Centre, Chinese Geological Survey, Chengdu 610081, China
Zheng Liu
Affiliation:
School of Resource Environment and Earth Science, Yunnan University, Yunnan 650091, China
*
Author for correspondence: Dong-Bing Wang, Email: wangdb06@163.com
Get access Rights & Permissions [Opens in a new window]

Abstract

This paper presents new LA-ICP-MS zircon U–Pb chronology, whole-rock geochemical and zircon Hf isotopic data for the felsic lavas of the Huili Group from the southwestern Yangtze Block. LA-ICP-MS zircon U–Pb dating shows that these rocks were emplaced in Late Mesoproterozoic time (∼1028 to 1019 Ma). Relative to typical I-type and S-type granitoids, all the samples are characterized by low Sr and Eu, and high high-field-strength element contents, high TFeO/MgO, enriched rare earth element compositions and negative Eu anomalies, indicating that they share the geochemical signatures of A-type granitoid. They can be further divided into two groups: Group I and Group II. Group I are A1-type felsic rocks and were produced by fractional crystallization of alkaline basaltic magmas. The Group II felsic lavas belong to the A2-type and were derived by partial melting of a crustal source with mixing of mantle-derived magmas. Both Group I and Group II felsic lavas may erupt in a continental back-arc setting. The coexistence of A1- and A2-type rocks in the southwestern Yangtze Block suggests that they can occur in the same tectonic setting.

Keywords

A-typeback-arc settingLate MesoproterozoicWestern Yangtze Block
Type
Original Article
Information
Geological Magazine , Volume 156 , Issue 8 , August 2019 , pp. 1425 - 1439
Copyright
© Cambridge University Press 2019 

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

Andersen, T (2002) Correction of common lead in U–Pb analyses that do not report 204Pb. Chemical Geology 192, 59–79.CrossRefGoogle Scholar
Bédard, JH (1999) Petrogenesis of boninites from the Betts Cove ophiolite, Newfoundland, Canada: identification of subducted source components. Journal of Petrology 40, 1853–89.CrossRefGoogle Scholar
Black, LP and Gulson, BL (1978) The age of the Mud Tank carbonatite, Strangways Range, Northern Territory. BMR Journal of Australian Geology and Geophysics 3, 227–32.Google Scholar
Bonin, B (2007) A-type granites and related rocks: evolution of a concept, problems and prospects. Lithos 97, 1–29.CrossRefGoogle Scholar
Bouvier, A, Vervoort, JD and Patchett, PJ (2008) The Lu–Hf and Sm–Nd isotopic composition of CHUR: constraints from unequilibrated chondrites and implications for the bulk composition of terrestrial planets. Earth and Planetary Science Letters 273, 48–57.CrossRefGoogle Scholar
Brown, GC, Thorpe, RS and Webb, PC (1984) The geochemical characteristics of granitoids in contrasting arcs and comments on magma sources. Journal of the Geological Society, London 141, 413–26.CrossRefGoogle Scholar
Cawood, PA, Zhao, GC, Yao, JL, Wang, W, Xu, YJ and Wang, YJ (2018) Reconstructing South China in Phanerozoic and Precambrian supercontinents. Earth-Science Reviews 186, 173–94.CrossRefGoogle Scholar
Chappell, BW and White, AJR (1974) Two contrasting granite types. Pacific Geology 8, 173–4.Google Scholar
Chen, JF, Foland, KA, Xing, FM, Xu, X and Zhou, TX (1991) Magmatism along the southeast margin of the Yangtze and Cathaysia block of China. Geology 19, 815–18.Google Scholar
Chen, LH, Zeng, G, Hu, SL, Yu, X and Chen, XY (2012) Crustal recycling and genesis of continental alkaline basalts: case study of the Cenozoic alkaline basalts from Shandong Province, Eastern China. Geological Journal of China Universities 18, 16–27 (in Chinese with English abstract).Google Scholar
Chen, WT, Sun, W-H, Wang, W, Zhao, J-H and Zhou, M-F (2014) “Grenvillian” intraplate mafic magmatism in the southwestern Yangtze Block, SW China. Precambrian Research 242, 138–53.CrossRefGoogle Scholar
Clemens, JD, Holloway, JR and White, AJR (1986) Origin of an A-type granite; experimental constraints. American Mineralogist 71, 317–24.Google Scholar
Collins, WJ, Beams, SD, White, AJR and Chappell, BW (1982) Nature and origin of A-type granites with particular reference to southeastern Australia. Contributions to Mineralogy and Petrology 80, 189–200.CrossRefGoogle Scholar
Creaser, RA, Price, RC and Wormald, RJ (1991) A-type granites revisited: assessment of a residual-source model. Geology 19, 163–6.2.3.CO;2>CrossRefGoogle Scholar
Deng, H, Peng, SB, Polat, A, Kusky, T, Jiang, XF, Han, QS, Wang, L, Huang, Y, Wang, JP, Zeng, W and Hu, ZX (2017) Neoproterozoic IAT intrusion into Mesoproterozoic MOR Miaowan ophiolite, Yangtze Craton: evidence for evolving tectonic settings. Precambrian Research 289, 75–94.CrossRefGoogle Scholar
Eby, GN (1990) The A-type granitoids: a review of their occurrence and chemical characteristics and speculations on their petrogenesis. Lithos 26, 115–34.CrossRefGoogle Scholar
Eby, GN (1992) Chemical subdivision of the A-type granitoids: petrogenetic and tectonic implications. Geology 20, 641–4.2.3.CO;2>CrossRefGoogle Scholar
Farmer, GL (2003) Continental basaltic rocks. In The Crust (ed. Rudnick, RL), pp. 85–121. Treatise on Geochemistry, Vol. 3. Oxford: Elsevier-Pergamon.Google Scholar
Frost, CD and Frost, BR (1997) Reduced rapakivi-type granites: the tholeiite connection. Geology 25, 647–50.2.3.CO;2>CrossRefGoogle Scholar
Gao, JF, Lu, JJ, Lai, MY, Lin, YP and Pu, W (2003) Analysis of trace elements in rock samples using HR-ICPMS. Journal of Nanjing University (Natural Sciences) 39, 844–50 (in Chinese with English abstract).Google Scholar
Greentree, MR, Li, Z-X, Li, X-H and Wu, H (2006) Late Mesoproterozoic to earliest Neoproterozoic basin record of the Sibao orogenesis in western South China and relationship to the assembly of Rodinia. Precambrian Research 151, 79–100.CrossRefGoogle Scholar
He, ZY and Xu, XS (2012) Petrogenesis of the Late Yanshanian mantle-derived intrusions in southeastern China: response to the geodynamics of paleo-Pacific plate subduction. Chemical Geology 328, 208–21.CrossRefGoogle Scholar
Hu, PY, Zhai, QG, Wang, J, Tang, Y and Ren, GM (2017) The Shimian ophiolite in the western Yangtze Block, SW China: zircon SHRIMP U–Pb ages, geochemical and Hf–O isotopic characteristics, and tectonic implications. Precambrian Research 298, 107–22.CrossRefGoogle Scholar
Jackson, SE, Pearson, NJ, Griffin, WL and Belousova, EA (2004) The application of laser ablation-inductively coupled plasma-mass spectrometry to in situ U–Pb zircon geochronology. Chemical Geology 211, 47–69.CrossRefGoogle Scholar
Jiang, GQ, Sohl, LE and Christie-Blick, N (2014) Neoproterozoic stratigraphic comparison of the Lesser Himalaya (India) and Yangtze Block (South China): paleogeographic implications. Geology 31, 917–20.CrossRefGoogle Scholar
Jiang, YH, Wang, GC, Liu, Z, Ni, CY, Qing, L and Zhang, Q (2015) Repeated slab advance-retreat of the Palaeo-Pacific plate underneath SE China. International Geology Review 57, 472–91.CrossRefGoogle Scholar
Jiang, YH, Zhao, P, Zhou, Q, Liao, SY and Jin, GD (2011) Petrogenesis and tectonic implications of early cretaceous S- and A-type granites in the northwest of the Gan-Hang rift, SE China. Lithos 121, 55–73.CrossRefGoogle Scholar
Li, ZX, Li, XH, Zhou, H and Kinny, PD (2002) Grenvillian continental collision in South China: new SHRIMP U–Pb zircon results and implications for the configuration of Rodinia. Geology 30, 163–6.2.0.CO;2>CrossRefGoogle Scholar
Li, XH, Zhou, GQ, Zhao, JX, Fanning, CM and Compston, W (1994) SHRIMP ion microprobe zircon U–Pb age and Sm–Nd isotopic characteristics of the NE Jiangxi ophiolite and its tectonic implications. Chinese Journal of Geochemistry 13, 317–25.Google Scholar
Liu, Z, Jiang, YH, Jia, RY, Zhao, P, Zhou, Q, Wang, GC and Ni, CY (2014) Origin of middle Cambrian and late Silurian potassic granitoids from the western Kunlun orogen, northwest China: a magmatic response to the Proto-Tethys evolution. Mineralogy and Petrology 108, 91–110.CrossRefGoogle Scholar
Liu, Z, Zhou, Q, Lai, Y, Qing, CS, Li, YX, Wu, JY and Xia, XB (2015) Petrogenesis of the early Cretaceous Laguila bimodal intrusive rocks from the Tethyan Himalaya: implications for the break-up of Eastern Gondwana. Lithos 236–237, 190–202.CrossRefGoogle Scholar
Loiselle, MC and Wones, DR (1979) Characteristics of anorogenic granites. Geological Society of America Abstracts with Programs 11, 468.Google Scholar
Patiño Douce, AE (1997) Generation of metaluminous A-type granites by low-pressure melting of calc-alkaline granitoids. Geology 25, 743–6.2.3.CO;2>CrossRefGoogle Scholar
Pearce, JA (1996) Sources and settings of granitic rocks. Episodes 19, 120–5.Google Scholar
Pearce, JA, Harris, NBW and Tindle, AG (1984) Trace element discrimination diagrams for the tectonic interpretation of granitic rocks. Journal of Petrology 25, 956–83.CrossRefGoogle Scholar
Poitrasson, F, Duthou, J-L and Pin, C (1995) The relationship between petrology and Nd isotopes as evidence for contrasting anorogenic granite genesis: example of the Corsican Province. Journal of Petrology 36, 1251–74.CrossRefGoogle Scholar
Pu, W, Gao, JF, Zhao, KD, Ling, HF and Jiang, SY (2005) Separation method of Rb–Sr, Sm–Nd using DCTA and HIBA. Journal of Nanjing University (Natural Sciences) 41, 445–50 (in Chinese with English abstract).Google Scholar
Pu, W, Zhao, KD, Ling, HF and Jiang, SY (2004) High precision Nd isotope measurement by Triton TI mass spectrometry. Acta Geoscientica Sinica 25, 271–4 (in Chinese with English abstract).Google Scholar
Qiu, XF, Ling, WL, Liu, XM, Kusky, T, Berkana, W, Zhang, YH, Gao, YJ, Lu, SS, Kuang, H and Liu, CX (2011) Recognition of Grenvillian volcanic suite in the Shennongjia region and its tectonic significance for the South China Craton. Precambrian Research 191, 101–19.CrossRefGoogle Scholar
Ren, GM, Pang, WH, Pan, GT, Wang, LQ, Sun, ZM, Yin, FG, Cui, XZ, Wang, DB, Deng, Q and Ren, F (2017) Ascertainment of the Mesoproterozoic Caiziyuan ophiolitic mélange on the western margin of the Yangtze Block and its geological significance. Geological Bulletin of China 36, 2061–75.Google Scholar
Rudnick, RL and Gao, S (2003) Composition of the continental crust. In The Crust (ed. Rudnick, RL), pp. 1–64. Treatise on Geochemistry, Vol. 3. Oxford: Elsevier-Pergamon.Google Scholar
Shellnutt, JG and Jahn, BM (2010) Formation of the late Permian Panzhihua plutonic-hypabyssal-volcanic igneous complex: implications for the genesis of Fe-Ti oxide deposits and A-type granites of SW China. Earth and Planetary Science Letters 289, 509–19.CrossRefGoogle Scholar
Shellnutt, JG and Zhou, MF (2007) Permian peralkaline, peraluminous and metaluminous A-type granites in the Panxi district, SW China: their relationship to the Emeishan mantle plume. Chemical Geology 243, 286–316.CrossRefGoogle Scholar
Smith, RE and Smith, SE (1976) Comments on the use of Ti, Zr, Y, Sr, K, P and Na in classification of basaltic magmas. Earth and Planetary Science Letters 32, 114–20.CrossRefGoogle Scholar
Steizner, M, Li, GX, Qian, Y, Zhu, MY and Erdtmann, BD (2007) Neoproterozoic to early Cambrian small shelly fossil assemblages and a revised biostratigraphic correlation of the Yangtze Platform (China). Palaeogeography, Palaeoclimatology, Palaeoecology 254, 67–99.CrossRefGoogle Scholar
Suárez, M and Pettigrew, TH (1976) An upper Mesozoic island-arc-back-arc system in the southern Andes and South Georgia. Geological Magazine 113, 305–400.CrossRefGoogle Scholar
Sun, J, Liu, Z, Zhang, S, Li, XG and Qi, JF (2017) Large-scale removal of lithosphere underneath the North China Craton in the Early Cretaceous: geochemical constraints from volcanic lavas in the Bohai Bay Basin. Lithos 292–293, 69–80.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
Turner, SP, Foden, JD and Morrison, RS (1992) Derivation of some A-type magmas by fractionation of basaltic magma: an example from the Padthaway Ridge, South Australia. Lithos 28, 151–79.CrossRefGoogle Scholar
Vervoort, J, Patchett, PJ, Blichert-Toft, J and Albarede, F (1999) Relationships between Lu–Hf and Sm–Nd isotopic systems in the global sedimentary system. Earth and Planetary Science Letters 168, 79–99.CrossRefGoogle Scholar
Wang, XL, Zhao, GC, Zhou, JC, Liu, YS and Hu, J (2008) Geochronology and Hf isotopes of zircon from volcanic rocks of the Shuangqiaoshan Group, South China: implications for the Neoproterozoic tectonic evolution of the eastern Jiangnan orogen. Gondwana Research 14, 355–67.CrossRefGoogle Scholar
Wang, XL, Zhou, JC, Wan, YS, Kitajima, K, Wang, D, Bonamici, C, Qiu, JS and Sun, T (2013) Magmatic evolution and crustal recycling of Neoproterozoic strongly peraluminous granitoids from southern China: Hf and O isotopes in zircon. Earth and Planetary Science Letters 366, 71–82.CrossRefGoogle Scholar
Whalen, JB, Currie, KL and Chappell, BW (1987) A-type granites: geochemical characteristics, discrimination and petrogenesis. Contribution to Mineralogy and Petrology 95, 407–19.CrossRefGoogle Scholar
Williams, IS, Buick, A and Cartwright, I (1996) An extended episode of early Mesoproterozoic metamorphic fluid flow in the Reynold Region, central Australia. Journal of Metamorphic Geology 14, 29–47.CrossRefGoogle Scholar
Winchester, JA and Floyd, PA (1977) Geochemical discrimination of different magma series and their differentiation products using immobile elements. Chemical Geology 20, 325–43.CrossRefGoogle Scholar
Wu, FY, Yang, YH, Xie, LW, Yang, JH and Xu, P (2006) Hf isotopic compositions of the standard zircons and baddeleyites used in U–Pb geochronology. Chemical Geology 234, 105–26.CrossRefGoogle Scholar
Xu, XS, Griffin, WL, Ma, X, O’Reilly, SY, He, ZY and Zhang, CL (2009) The Taihua group on the southern margin of the North China craton: further insights from U–Pb ages and Hf isotope compositions of zircons. Mineralogy and Petrology 97, 43–59.CrossRefGoogle Scholar
Yan, LL, He, ZY, Beier, C and Klemd, R (2018) Geochemical constraints on the link between volcanism and plutonism at the Yunshan caldera complex, SE China. Contributions to Mineralogy and Petrology 173, 4.CrossRefGoogle Scholar
Zeng, G, Chen, LH, Hofmann, AW, Jiang, SY and Xu, XS (2011) Crust recycling in the sources of two parallel volcanic chains in Shandong, North China. Earth Planetary Sciences Letters 302, 359–68.CrossRefGoogle Scholar
Zeng, G, Chen, LH, Hu, SL and Xu, XS (2013) Genesis of Cenozoic low-Ca alkaline basalts in the Nanjing basaltic field, eastern China: the case for mantle xenolith-magma interaction. Geochemistry, Geophysics, Geosystems 14, 1660–77.CrossRefGoogle Scholar
Zeng, G, Chen, LH, Xu, XS, Jiang, SY and Hofmann, AW (2010) Carbonated mantle sources for Cenozoic intra-plate alkaline basalts in Shandong, North China. Chemical Geology 273, 35–45.CrossRefGoogle Scholar
Zeng, G, He, ZY, Li, Z, Xu, XS and Chen, LH (2016) Geodynamics of paleo-Pacific plate subduction constrained by the source lithologies of Late Mesozoic basalts in southeastern China. Geophysical Research Letters 43, 10189–97.CrossRefGoogle Scholar
Zhang, CL, Santosh, M, Zou, HB, Li, HK and Huang, WC (2013) The Fuchuan ophiolite in Jiangnan Orogen: geochemistry, zircon U–Pb geochronology, Hf isotope and implications for the Neoproterozoic assembly of South China. Lithos 179, 263–74.CrossRefGoogle Scholar
Zhang, SB, Wu, RX and Zheng, YF (2012) Neoproterozoic continental accretion in South China: geochemical evidence from the Fuchuan ophiolite in the Jiangnan orogen. Precambrian Research 220–221, 45–64.CrossRefGoogle Scholar
Zhao, G (2015) Jiangnan Orogen in South China: developing from divergent double subduction. Gondwana Research 27, 1173–80.CrossRefGoogle Scholar
Zhao, G and Cawood, PA (2012) Precambrian geology of China. Precambrian Research 222–223, 13–54.CrossRefGoogle Scholar
Zhou, Q, Liu, Z, Lai, Y, Wang, GC, Liao, ZW, Li, YX, Wu, JY, Wang, SW and Qing, CS (2018) Petrogenesis of mafic and felsic rocks from the Comei large igneous province, South Tibet: implications for the initial activity of the Kerguelen plume. Geological Society of America Bulletin 130, 811–24.CrossRefGoogle Scholar
Zhou, XM, Zou, HB, Yang, JD and Wang, YX (1989) Sm–Nd isochron age of the Fuchuan Ophiolite Suite in Shexian, Anhui Provence and its geological significance. China Science Bulletin 16, 1243–5.Google Scholar
Zhu, WG, Zhong, H, Li, ZX, Bai, ZJ and Yang, YJ (2016) SIMS zircon U–Pb ages, geochemistry and Nd–Hf isotopes of ca. 1.0 Ga mafic dykes and volcanic rocks in the Huili area, SW China: origin and tectonic significance. Precambrian Research 273, 67–89.CrossRefGoogle Scholar
Supplementary material: File

Wang et al. supplementary material

Table S1

Download Wang et al. supplementary material(File)
File 50.1 KB