Paleo - position of the South China Craton in the Rodinia Supercontinent: Evidence from the U - Pb age and Hf isotope of detrital zircon from the Nam Co Complex

  • Affiliations:

    1 Hanoi University of Mining and Geology, Hanoi, Vietnam
    2 Central for Excellence in Analyses and Experiment, Hanoi, Vietnam
    3 Chungbuk National University, Cheongju, Korea

  • *Corresponding:
    This email address is being protected from spambots. You need JavaScript enabled to view it.
  • Received: 11st-Jan-2021
  • Revised: 23rd-Apr-2021
  • Accepted: 21st-May-2021
  • Online: 30th-June-2021
Pages: 1 - 12
Views: 2823
Downloads: 1260
Rating: 1.0, Total rating: 124
Yours rating

Abstract:

To constrain the paleo - positions of the South China Cratons in the Rodinia Supercontinent during the Neoproterozoic, the in - situ U - Pb dating, and Hf isotope analysis of the detrital zircon from the Nam Co Complex, Song Ma Suture zone, northwestern Vietnam was performed. The U - Pb isotopic dating on detrital zircons shows that the Nam Co Complex demonstrates the major population (>50%) of around ~850 Ma while the minor population is scattered between ~1.2÷3.0 Ga. The Neoproterozoic age spectrum exhibits a large range of the εHf(t) from strongly negative to positive values ( - 17.418022÷ 14.600527), indicating that the source of the magma for this age range has been not only derived from reworking of the Archean basement rocks, but also generated from the juvenile material. The U - Pb age distribution patterns and Hf isotopic data of the detrital zircon in the Nam Co Complex are compatible with those of the South China Craton rather than those of the Indochina Craton. The data also indicate that sedimentary protoliths of the Nam Co Complex were deposited in a convergent - related basin along the southwestern margin of the South China Craton during the Neoproterozoic. Combined with the similarities of the detrital zircon age between western Cathaysia, Indochina, East Antarctica and East India, it is proved that the South China Craton was situated at the margin of the Rodinia Supercontinent and in close proximity to the Indochina, East Antarctica and East India.

How to Cite
., H.Vinh Bui and Kim, Y. 2021. Paleo - position of the South China Craton in the Rodinia Supercontinent: Evidence from the U - Pb age and Hf isotope of detrital zircon from the Nam Co Complex. Journal of Mining and Earth Sciences. 62, 3 (Jun, 2021), 1-12. DOI:https://doi.org/10.46326/JMES.2021.62(3).01.
References

Andersen, T., (2002). Correction of common lead in U - Pb analyses that do not report 204Pb. Chemical Geology 192. 59 - 79.

Boger, S. D., Carson, C. J., Wilson, C. J. L., Fanning, C. M., (2000). Neoproterozoic deformation in the Radok Lake region of the northern Prince Charles Mountains, east Antarctica; evidence for a single protracted orogenic event. Precambrian Research, 104. 1 - 24.

Bose, S., Dunkley, D. J., Arima, M., (2011). India­Antarctica AustraliaLaurentia connection in the Paleoproterozoic - Mesoproterozoic revisited: Evidence from new zircon U Pb and monazite chemical age data from the Eastern Ghats Belt, India. Geological Society of America Bulletin, 123. 2031 - 2049.

Cai, Y. F., Wang, Y. J., Cawood, P. A., Fan, W. M., Liu, H., Xing, X. W., Zhang, Y., (2014). Neoproterozoic subduction along the Ailaoshan zone, South China: geochronological and geochemical evidence from amphibolite. Precambrian Research, 245. 13 - 28.

Carson, C. J., Ague, J. J., Coath, C. D., (2002). U - Pb geochronology from Tonagh  of the Napier Complex. Precambrian Research, 116. 27 - 263.

Cawood, P. A., Nemchin, A. A., (2000). Provenance record of a rift basin: U/Pb ages of detrital zircons from the Perth Basin, Western Australia. Sedimentary Geology, 134. 209 - 234.

Cawood, P. A., Wang, Y. J., Xu, Y. J., Zhao, G. C., (2013). Locating South China in Rodinia and Gondwana: a fragment of greater India lithosphere?. Geology, 41. 903 - 906.

Chu, N. C., Taylor, R. N., Chavagnac, V., Nesbitt, R. W., Boella, M., Milton, J. A., (2002). Hf isotope ratio analysis using multi - collector inductively coupled plasma mass spectrometry: an evaluation of isobaric interference corrections. Journal of Analytical Atomic Spectrometry, 17. 1567 - 1574.

Dong, Y. P., Liu, X. M., Santosh, M., Chen, Q., Zhang, X. N., Li, W., He, D. F., Zhang, G. W., (2012). Neoproterozoic accretionary tectonics along the northwestern margin of the Yangtze Block, China: constraints from zircon U - Pb geochronology and geochemistry. Precambrian Research, 196. 247 - 274.

Dong, Y. P., Liu, X. M., Santosh, M., Zhang, X. N., Chen, Q., Yang, C., Yang, Z., (2011). Neoproterozoic subduction tectonics of the northwestern Yangtze Block in South China: constrains from zircon U - Pb geochronology and geochemistry of mafic intrusions in the Hannan Massif. Precambrian Research, 189. 66 - 90.

Griffin, W. L., Belousova, E. A., Shee, S. R., Pearson, N. J., O'Reilly, S. Y., (2004). Archean crustal evolution in the northern YilgarnCraton: U - Pb and Hf - isotope evidence from detrital zircons. Precambrian Research 131. 231 - 282.

Griffin, W. L., Pearson, N. J., Belousova, E., Jackson, S. E., van Achterbergh, E., O’Reilly, S. Y., Shee, S. R., (2000). The Hf isotope composition of Cratonic mantle: LAM - MC - ICPMS analysis of zircon megacrysts in kimberlites. Geochim. Cosmochim. Acta. 64. 133 - 147.

Hau, B. V., Kim, Y., Thanh, N. X., Hai, T. T., Yi, K., (2018). Neoproterozoic deposition and Triassic metamorphism of metasedimentary rocks in the Nam Co Complex, Song Ma Suture Zone, NW Vietnam. Geosciences Journal, 22. 459 - 568.

Hoffman, F. P., (1991). Did breakout of Laurentia turn Gondwana inside - out?. Science, 252. 1409 - 1411.

Kelly, N. M., Clarke, G. L., Fanning, C. M., (2002). A two - stage evolution of the Neoproterozoic Rayner Structural Episode: new U - Pb sensitive high resolution ion microprobe constraints from the Oygarden Group, Kemp Land, East Antarctica. Precambrian Research, 116. 307 - 330.

Kemp, A. I. S., Hawkesworth, C. J., Collins, W. J., Gray, C. M., Blevin, P. L., ( 2009). Isotopic evidence for rapid continental growth in an extensional accretionary orogen: The Tasmanides, eastern Australia. Earth and Planetary Science Letters, 284. 455 - 466

Laskowski, A. K., Decelles, P. G., Gehrels, G. E., (2013). Detrital zircon geochronology of Cordilleran retroarc foreland basin strata, western North America. Tectonics, 32. 1027 - 1048.

Li, X. H., (1999). U - Pb zircon ages of granites from the southern margin of the Yangtze Block: timing of the Neoproterozoic Jinning Orogeny in SE China and implications for Rodinia Assembly. Precambrian Research. 43 - 57.

Li, X. H., Li, Z. X., Sinclair, J. A., Li, W. X., Carter, G., (2006). Revisiting the “Yanbian Terrane”: implications for Neoproterozoic tectonic evolution of the western Yangtze Block, South China. Precambrian Research, 151. 14 - 30.

Li, Z. X., Li, X. H., 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 - 182.

Li, Z. X., Li, X. H., Zhou, H., Kinny, P. D., (2002). Grenvillian continental collision in southChina: New SHIMP U - Pb zircon results and implications for the configurationof Rodinia. Geology, 30. 163 - 166.

Li, Z. X., Zhang, L., Powell, C. M., (1995). South China in Rodinia: part of the missing linkbetween Australia - East Antarctica and Laurentia? Geology, 23. 407 - 410

Ling, W. L., Gao, S., Zhang, B. R., Li, H. M., Liu, Y., Cheng, J. P., (2003). Neoproterozoic tectonic evolution of the northwestern Yangtze Craton, South China: implications for amalgamation and break - up of the RodiniaSupercontinent. Precambrian Research, 122. 111 - 140.

Liu, R., Zhou, H., Zhang, L., Zhong, Z., Zeng, W., Xiang, H., Jin, S., Lu, X., Li, C., (2009). Paleoproterozoic reworking of ancient crust in the Cathaysia Block, South China: evidence from zircon trace elements, U - Pb and Lu - Hf isotopes. Chinese Science Bulletin, 54, 1543 - 1554.Ludwig, K. R., (2008). User’s manual for Isoplot 3.6: a geo - chronological toolkit for Microsoft Excel. Berkeley Geochronology Center, Special Publication, 4. 77p.

Qi, X. X., Zeng, L. S., Zhu, L. H., Hu, Z. C., Hou, K. J., (2012). Zircon U - Pb and Lu - Hf isotopic systematics of the Daping plutonic rocks: implications for the Neoproterozoic tectonic evolution of the northeastern margin of the Indochina block, Southwest China. Gondwana Research, 21. 180 - 193.

Saha, S., Das, K., Hidaka, H., Kimura, K., Pratim, P., Chakraborty, P.P., Hayasaka, Y., (2016). Detrital zircon geochronology (U - Pb SHRIMP and LA - ICPMS) from the Ampani Basin, Central India: Implication for provenance and Mesoproterozoic tectonics at East Indian Cratonic margin. Precambrian Research, 281. 363 - 383.

Sircombe, K. N., Freeman, M. J., (1999). Provenance of detrital zircon on the Western Australian coastline - Implications for the geological history of the Perth basin and denudation of the YilgarnCraton. Geology, 27. 879 - 882.

Sláma, J., Košler, J., Condon, D. J., Crowley, J. L., Gerdes, A.,Hanchar, J. M., Horstwood, M. S. A., Morris, G. A., Nasdala, L., Norberg, N., Schaltegger, U., Schoene, B., Tubrett, M. N., Whitehouse, M. J., (2008). Plešovice zircon - A new natural reference material for U - Pb and Hf isotopic microanalysis. Chemical Geology, 1 - 2. 1 - 35.

Sun, W. H., Zhou, M. F., Gao, J. F., Yang, Y. H., Zhao, X. F., Zhao, J. H., (2009). Detrital zircon U - Pb geochronological and Lu - Hf isotopic constraints on the Precambrian magmatic and crustal evolution of the western Yangtze Block, SW China. Precambrian Research 172. 99 - 126.

Sun, W. H., Zhou, M. F., Yan, D. P., Li, J. W., Ma, Y. X., 92008). Provenance and tectonic setting of the Neoproterozoic Yanbian Group, western Yangtze Block (SW China). Precambrian Research, 167. 213 - 236.

Usuki, T., Lan, C. Y., Wang, K. L., Chiu, Y., (2013). Linking the Indochina block and Gondwana during the Early Paleozoic: evidence from U - Pb ages and Hf isotopes of detrital zircons. Tectonophysics, 586. 145 - 159.

Veevers, J. J., Saeed, A., Belousova, E. A., Griffin, W. L., (2005), U - Pb ages and source composition by Hf - isotope and trace - element analysis of detrital zircons in Permian sandstone and modern sand from southwestern Australia anda review of the paleogeographical and denudational history of the YilgarnCraton. Earth - Science Reviews, 68. 245 - 279.

Vervoort, J. D., Patchett, P. J., Söderlund, U., Baker, M., (2004). Isotopic composition of Yb and the determination of Lu concentrations and Lu/Hf ratios by isotope dilution using MC - ICPMS. Geochem. Geophys. Geosystem. 5. 1 - 15.

Wang, L. J., Yu, J. H., Griffin, W. L., O'Reilly, S. Y., (2012). Early crustal evolution in the western Yangtze Block: evidence from U - Pb and Lu - Hf isotopes on detrital zircons from sedimentary rocks. Precambrian Research, 222 - 223. 368 - 385.

Wang, Y., Zhang, A., Cawood, P. A., Fan, W., Xu, J., Zhang, G., Zhang, Y.,(2013). Geochronological, geochemical and Nd - Hf - Os isotopic fingerprinting of an early Neoproterozoic arc - back - arc system in South China and its accretionary assembly along the margin of Rodinia. Precambrian Research, 231. 343 - 371.

Wiedenbeck, M., Allé, P., Corfu, F., Griffin, W. L., Meier, M., Oberli, F., von Quadt, A., Roddick, J. C., Spiegel, W., (1995). Three natural zircon standards for U - Th - Pb, Lu - Hf, trace element and REE analyses. Geostandards Newsletter 19. 1 - 23.

Xia, Y., Xu, X. S., Zhu, K. Y., (2012). Paleoproterozoic S - and A - type granites in southwestern Zhejiang: magmatism, metamorphism and implications for the crustal evolution of the Cathaysia basement. Precambrian Research, 216 - 219. 177 - 207.

Xiao, L., Zhang, H. F., Ni, P. Z., Xiang, H., Liu, X. M., (2007). LA - ICP - MS U - Pb zircon geochronology of early Neoproterozoic mafic - intermediate intrusions from NW margin of the Yangtze Block, South China: implications for tectonic evolution. Precambrian Research, 154. 221 - 235.

Yu, J. H., O'Reilly, S. Y., Wang, L., Griffin, W. L., Zhang, M., Wang, R., Jiang, S., Shu, L., (2008). Where was South China in the RodiniaSupercontinent? evidence from U - Pb geochronology and Hf isotopes of detrital zircons. Precambrian Research, 164. 1 - 15.

Yu, J. H., O'Reilly, S. Y., Wang, L., Griffin, W. L., Zhou, M. F., Zhang, M., Shu, L., (2010). Components and episodic growth of Precambrian crust in the Cathaysia Block, South China: evidence from U - Pb ages and Hf isotopes of zircons in Neoproterozoic sediments. Precambrian Research, 181. 97 - 114.

Zhang, S. B., Zheng, Y. F., Wu, Y. B., Zhao, Z. F., Gao, S., Wu, F. Y., (2006). Zircon U - Pb age and Hf isotope evidence for 3.8 Ga crustal remnant and episodic reworking of Archean crust in South China. Earth and Planetary Science Letters, 252. 56 - 71.

Zhang, Y., Wang, Y., Zhang, Y., Zhang, A., (2015). Neoproterozoic assembly of the Yangtze and Cathaysia blocks: Evidence from the Cangshuipu Group and associated rocks along the Central Jiangnan Orogen, South China. Precambrean Research, 269. 18 - 30.

Zhao, J. H., Zhou, M. F., (2007). Geochemistry of Neoproterozoic mafic intrusions in the Panzhihua district (Sichuan Province, South China): implications for subduction - related metasomatism in the upper mantle. Precambrian Research, 152. 27 - 47.

Zheng, J., Griffin, W. L., O’Reilly, S. Y., Zhang, M., Pearson, N., Yuanming, P.,( 2006). Widespread Archean basement beneath the Yangtze Craton. Geological Society of America Bulletin, 34. 417 - 420.

Zheng, Y., (2004). Position of South China in configuration of Neoproterozoic Supercontinent. Chinese Science Bulletin 49. 751 - 753.

Other articles