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Zircon U–Pb geochronology of the Zanhuang metamorphic complex: reappraisal of the Palaeoproterozoic amalgamation of the Trans-North China Orogen

Published online by Cambridge University Press:  30 April 2013

LING-LING XIAO ,
GUO-DONG WANG ,
HAO WANG ,
ZONG-SHENG JIANG ,
CHUN-RONG DIWU  and
CHUN-MING WU
LING-LING XIAO*
Affiliation:
Institute of Geology, Chinese Academy of Geological Sciences, 26 Baiwanzhuang Street, Beijing 100037, China College of Earth Science, University of Chinese Academy of Sciences, Beijing 100049, China
GUO-DONG WANG
Affiliation:
College of Earth Science, University of Chinese Academy of Sciences, Beijing 100049, China
HAO WANG
Affiliation:
College of Earth Science, University of Chinese Academy of Sciences, Beijing 100049, China
ZONG-SHENG JIANG
Affiliation:
College of Earth Science, University of Chinese Academy of Sciences, Beijing 100049, China Institute of Mineral Resources, Chinese Academy of Geological Sciences, 26 Baiwanzhuang Street, Beijing 100037, China
CHUN-RONG DIWU
Affiliation:
State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an 710069, China
CHUN-MING WU
Affiliation:
College of Earth Science, University of Chinese Academy of Sciences, Beijing 100049, China
*
†Author for correspondence: [email protected]
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Abstract

Amphibolites and metapelites exposed in the Zanhuang metamorphic complex situated in the south-middle section of the Trans-North China Orogen (TNCO) underwent upper-amphibolite-facies metamorphism and record clockwise P–T paths including retrograde isothermal decompression. High-resolution zircon U–Pb geochronological analyses indicate that the metamorphic peak occurred during ~ 1840–1860 Ma, which is in accordance with the ubiquitous metamorphic ages of ~ 1850 Ma retrieved by miscellaneous geochronologic methods throughout the metamorphic terranes of the northern TNCO, confirming that the south-middle section of the TNCO was involved in the amalgamation of the Eastern and Western Blocks of the North China Craton during the Palaeoproterozoic.

Keywords

SIMS datingLA-ICP-MS datingzirconZanhuang metamorphic complexNorth China Craton
Type
Rapid Communication
Information
Geological Magazine , Volume 150 , Issue 4 , July 2013 , pp. 756 - 764
Copyright
Copyright © Cambridge University Press 2013 

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References

Ernst, W. G. 1988. Tectonic history of subduction zones inferred from retrograde blueschist P-T paths. Geology 16, 1081–4.2.3.CO;2>CrossRefGoogle Scholar
Guo, J. H., Bian, A. G. & Shi, X. 1996. High-pressure granulite, retrograde eclogite and granite: early Precambrian Sanggan structure belt. In Granulites and Lower Continental Crust in North China Archaean Craton (ed. Zhai, M. G.), pp. 21–53. Beijing: Seismological Press.Google Scholar
Guo, J. H., O'Brien, P. J. & Zhai, M. G. 2002. High-pressure granulites in the Sanggan area, North China Craton: metamorphic evolution, P-T paths and geotectonic significance. Journal of Metamorphic Geology 20, 741–56.CrossRefGoogle Scholar
Guo, J. H., Sun, M., Chen, F. K. & Zhai, M. G. 2005. Sm–Nd and SHRIMP U–Pb zircon geochronology of high-pressure granulites in the Sanggan area, North China Craton: timing of Paleoproterozoic continental collision. Journal of Asian Earth Sciences 24, 629–42.CrossRefGoogle Scholar
Guo, J. H., Zhai, M. G., Li, Y. G. & Li, J. H. 1999. Metamorphism, PT paths and tectonic significance of garnet amphibolite and granulite from Hengshan, North China Craton. Scientia Geologica Sinica 34, 311–25 (in Chinese with English abstract).Google Scholar
Guo, J. H., Zhai, M. G., Li, Y. G. & Yan, Y. H. 1998. Contrasting metamorphic PT paths of Archaean high pressure granulites from the North China Craton: metamorphism and tectonic significance. Acta Petrologica Sinica 14, 430–48 (in Chinese with English abstract).Google Scholar
Kröner, A., Wilde, S. A., O'Brien, P. J., Li, J. H., Passchier, C. W., Walte, N. P. & Liu, D. Y. 2005. Field relationships, geochemistry, zircon ages and evolution of a late Archean to Paleoproterozoic lower crustal section in the Hengshan Terrain of Northern China. Acta Geologica Sinica 79, 605–29.Google Scholar
Kröner, A., Wilde, S. A., Zhao, G. C., O'Brien, P. J., Sun, M., Liu, D. Y., Wan, Y. S., Liu, S. W. & Guo, J. H. 2006. Zircon geochronology of mafic dykes in the Hengshan Complex of northern China: evidence for Late Palaeoproterozoic rifting and subsequent high pressure event in the North China Craton. Precambrian Research 146, 45–67.CrossRefGoogle Scholar
Li, Q. L., Li, X. H., Liu, Y., Tang, G. Q., Yang, J. H. & Zhun, W. G. 2010. Precise U–Pb and Pb–Pb dating of Phanerozoic baddeleyite by SIMS with oxygen flooding technique. Journal of Analytical Atomic Spectrometry 25, 1107–13.CrossRefGoogle Scholar
Li, X. H., Liu, Y., Li, Q. L., Guo, C. H. & Chamberlain, K. R. 2009. Precise determination of Phanerozoic zircon Pb/Pb age by multicollector SIMS without external standardization. Geochemistry, Geophysics, Geosystems 10, Q04010.Google Scholar
Liu, C. H., Zhao, G. C., Liu, F. L., Sun, M., Zhang, J. & Yin, C. Q. 2012. Zircons U-Pb and Lu-Hf isotopic and whole-rock geochemical constraints on the Gantaohe Group in the Zanhuang Complex: implications for the tectonic evolution of the Trans-North China Orogen. Lithos 146–147, 80–92.CrossRefGoogle Scholar
Liu, F. L. & Shen, Q. H. 1999. Retrogressive textures and metamorphic reaction features of Al-rich gneisses in the granulite facies belt from northwestern Hebei Province. Acta Petrologica Sinica 15, 505–17 (in Chinese with English abstract).Google Scholar
Liu, S. W. 1996. P–T path of granulites in the Fuping area. Geological Journal of China Universities 2, 75–84 (in Chinese).Google Scholar
Liu, S. W., Zhao, G. C., Wilde, S. A., Shu, G. M., Sun, M., Li, Q. G., Tian, W. & Zhang, J. 2006. Th–U–Pb monazite geochronology of the Lüliang and Wutai Complexes: constraints on the tectonothermal evolution of the Trans-North China Orogen. Precambrian Research 148, 205–24.CrossRefGoogle Scholar
Liu, S. W., Zhang, C., Liu, C. H., Li, Q. G., Lü, Y. J., Yu, S. Q., Tian, W. & Feng, Y. G. 2007. EPMA Th–U–Pb dating of monazite for Zhongtiao and Lüliang Precambrian metamorphic complexes. Earth Science Frontiers 14, 64–74 (in Chinese with English abstract).CrossRefGoogle Scholar
Liu, X. M., Gao, S., Diwu, C. R., Yuan, H. L. & Hu, Z. C. 2007. Simultaneous in-situ determination of U–Pb age and trace elements in zircon by LA ICP-MS in 20 μm spot size. Chinese Science Bulletin 52, 1257–64.CrossRefGoogle Scholar
Ludwig, K. R. 2003. Isoplot 3.0 – A Geochronological Toolkit for Microsoft Excel. Berkeley Geochronology Center, Special Publication, no. 4.Google Scholar
Ma, J. & Wang, R. M. 1994. Reviews in garnet–clinopyroxene geothermometers and geobarometers with their application to granulite: the comparison of Miyun (Zunhua) and Xuanhua granulite forming conditions. In Geological Evolution of the Granulite Terrane in North Part of the North China Craton (eds Qian, X. L. & Wang, R. M.), pp. 71–88. Beijing: Seismological Press (in Chinese with English abstract).Google Scholar
Mei, H. L. 1994. P–T–t path and tectonic evolution of Paleoproterozoic metamorphic rocks in Zhongtiaoshan area. Geological Review 40, 36–47 (in Chinese with English abstract).Google Scholar
O'Brien, P. J., Walte, N. & Li, J. H. 2005. The petrology of two distinct granulite types in the Hengshan Mts., China, and tectonic implications. Journal of Asian Earth Sciences 24, 615–27.CrossRefGoogle Scholar
Peng, P., Liu, F., Zhai, M. G. & Guo, J. H. 2012. Age of the Miyun dyke swarm: constraints on the maximum depositional age of the Changcheng System. Chinese Science Bulletin 57, 105–10.CrossRefGoogle Scholar
Peng, P., Zhai, M. G., Ernst, R. E., Guo, J. H., Liu, F. & Hu, B. 2008. A 1.78 Ga large igneous province in the North China craton: The Xiong'er Volcanic Province and the North China dyke swarm. Lithos 101, 260–80.CrossRefGoogle Scholar
Peng, P., Zhai, M. G. & Guo, J. H. 2006. 1.80–1.75 Ga mafic dyke swarms in the central North China craton: implications for a plume-related break-up event. In Dyke Swarms – Time Markers of Crustal Evolution (eds Hanski, E., Mertanen, S., Rämö, T. & Vuollo, J.), pp. 99–112. London: Taylor & Francis.Google Scholar
Peng, P., Zhai, M. G., Zhang, H. F. & Guo, J. H. 2005. Geochronological constraints on the Paleoproterozoic evolution of the North China Craton: SHRIMP zircon ages of different types of mafic dikes. International Geology Review 47, 492–508.CrossRefGoogle Scholar
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 249, 1–35.CrossRefGoogle Scholar
Spear, F. S., Hickmott, D. D. & Selverstone, J. 1990. Metamorphic consequences of thrust emplacement, Fall Mountain, New Hampshire. Geological Society of America Bulletin 102, 1344–60.2.3.CO;2>CrossRefGoogle Scholar
Spear, F. S., Kohn, M. J., Florence, F. & Menard, T. 1990. A model for garnet and plagioclase growth in politic schists: implications for thermobarometry and P-T path determinations. Journal of Metamorphic Geology 8, 683–96.CrossRefGoogle Scholar
Stacey, J. S. & Kramers, J. D. 1975. Approximation of terrestrial lead isotope evolution by a two-stage model. Earth and Planetary Science Letters 26, 207–21.CrossRefGoogle Scholar
Steiger, R. H. & Jäger, E. 1977. Subcommission on geochronology: convention on the use of decay constants in geo- and cosmochronology. Earth Planet Science Letters 36, 359–62.CrossRefGoogle Scholar
Tracy, R. J., Robinson, P. & Thompson, A. B. 1976. Garnet composition and zoning in the determination of temperature and pressure of metamorphism, central Massachusetts. American Mineralogist 61, 762–75.Google Scholar
Trap, P., Faure, M., Lin, W. & Monié, P. 2007. Late Palaeoproterozoic (1900–1800 Ma) nappe stacking and polyphase deformation in the Hengshan-Wutaishan area: implication for the understanding of the Trans-North China Belt, North China Craton. Precambrian Research 156, 85–106.CrossRefGoogle Scholar
Trap, P., Faure, M., Lin, W., Monié, P. & Bruguier, O. 2008. Contrasted tectonic styles for the Paleoproterozoic evolution of the North China Craton: evidence for a ~2.1Ga thermal and tectonic event in the Fuping Massif. Journal of Structural Geology 30, 1109–25.CrossRefGoogle Scholar
Trap, P., Faure, M., Lin, W., Monié, P., Meffre, S. & Melletton, J. 2009. The Zanhuang Massif, the second and eastern suture zone of the Paleoproterozoic Trans-North China Orogen. Precambrian Research 172, 80–98.CrossRefGoogle Scholar
Wan, Y. S., Wilde, S. A., Liu, D. Y., Yang, C. X., Song, B. & Yin, X. Y. 2006. Further evidence for ~1.85 Ga metamorphism in the central zone of the north China Craton: SHRIMP U–Pb dating of zircons from metamorphic rocks in the Lushan area, Henan Province. Gondwana Research 9, 189–97.CrossRefGoogle Scholar
Wang, R. M., Chen, Z. Z. & Chen, F. 1991. Grey tonalitic gneiss and high pressure granulite inclusions in Hengshan, Shanxi Province, and their geological significance. Acta Petrologica Sinica 7, 36–46 (in Chinese with English abstract).Google Scholar
Wang, Y. J., Fan, W. M., Guo, F. & Li, C. W. 2003 a. Biotite 40Ar/39Ar geochronology of the deformational rocks from Zanhuang metamorphic domain in southern Taihang mountains and their tectonothermal overprinting. Acta Petrologica Sinica 19, 131−40 (in Chinese with English abstract).Google Scholar
Wang, Y. J., Fan, W. M., Zhang, Y. & Guo, F. 2003 b. Structural evolution and 40Ar/39Ar dating of the Zanhuang metamorphic domain in the North China Craton: constraints on Paleoproterozoic tectonothermal overprinting. Precambrian Research 122, 159–82.CrossRefGoogle Scholar
Wang, Y. J., Fan, W. M., Zhang, Y. H., Guo, F., Zhang, H. F. & Peng, T. P. 2004. Geochemical, 40Ar/39Ar geochronological and Sr–Nd isotopic constraints on the origin of Paleoproterozoic mafic dikes from the southern Taihang Mountains and implications for the ca. 1800Ma event of the North China Craton. Precambrian Research 135, 55–77.CrossRefGoogle Scholar
Wang, Y. J., Zhao, G. C., Cawood, P. A., Fan, W. M., Peng, T. P. & Sun, L. H. 2008. Geochemistry of Paleoproterozoic (~1770 Ma) mafic dikes from the Trans-North China Orogen and tectonic implications. Journal of Asian Earth Sciences 33, 61–77.CrossRefGoogle Scholar
Wiedenbeck, M., Alle, P., Corfu, F., Griffin, W. L., Meier, M., Oberli, F., Vonquadt, A., Roddick, J. C. & Speigel, W. 1995. Three natural zircon standards for U–Th–Pb, Lu–Hf, trace-element and REE analyses. Geostandards Newsletter 19, 1–23.CrossRefGoogle Scholar
Xiao, L. L., Jiang, Z. S., Wan, G. D., Wan, Y. S., Wang, T. & Wu, C. M. 2011 a. Metamorphic reactions and metamorphic P–T paths of the Precambrian metamorphic complex, Zanhuang, Hebei, north China. Acta Petrologica Sinica 27, 980–1002 (in Chinese with English abstract).Google Scholar
Xiao, L. L., Wu, C. M., Zhao, G. C., Guo, J. H. & Ren, L. D. 2011 b. Metamorphic P–T paths of the Zanhuang amphibolitic gneisses and metapelitic gneisses: constraints on the tectonic evolution of the Paleoproterozoic Trans-North China Orogen. International Journal of Earth Sciences 100, 717–39.CrossRefGoogle Scholar
Yang, C. H., Du, L. L., Ren, L. D., Song, H. X., Wan, Y. S., Xie, H. Q. & Liu, Z. X. 2011. The age and petrogenesis of the Xuting Granite in the Zanhuang Complex, Hebei Province: constraints on the structural evolution of the Trans-North China Orogen, North China Craton. Acta Petrologica Sinica 27, 1003–16 (in Chinese with English abstract).Google Scholar
Zhai, M. G., Bian, A. G. & Zhao, T. P. 2000. The amalgamation of the supercontinent of North China craton at the end of the Neoarchaean, and its break-up during the late Palaeoproterozoic and Mesoproterozoic. Science in China (Series D) 43, 219–32.CrossRefGoogle Scholar
Zhai, M. G., Guo, J. H., Yan, Y. H., Han, X. L. & Li, Y. G. 1992. Discovery and preliminary study of the Archean high-pressure granulites in the North China. Science in China (Series B) 12, 1325–30 (in Chinese).Google Scholar
Zhao, G. C., Cawood, P. A. & Lu, L. Z. 1999. Petrology and P–T history of the Wutai amphibolites: implications for tectonic evolution of the Wutai Complex, China. Precambrian Research 93, 181–99.CrossRefGoogle Scholar
Zhao, G. C., Cawood, P. A., Wilde, S. A. & Lu, L. Z. 2001 a. High-pressure granulites (retrograded eclogites) from the Hengshan Complex, North China Craton: petrology and tectonic implications. Journal of Petrology 42, 1141–70.CrossRefGoogle Scholar
Zhao, G. C., Cawood, P. A., Wilde, S. A. & Sun, M. 2000 a. Metamorphism of basement rocks in the Central Zone of the North China Craton: implications for Paleoproterozoic tectonic evolution. Precambrian Research 103, 55–88.CrossRefGoogle Scholar
Zhao, G. C., Sun, M., Wilde, S. A. & Li, S. Z. 2005. Late Archean to Palaeoproterozoic evolution of the North China Craton: key issues revisited. Precambrian Research 136, 177–202.CrossRefGoogle Scholar
Zhao, G. C., Wilde, S. A., Cawood, P. A. & Lu, L. Z. 1998. Thermal evolution of the Archaean basement rocks from the eastern part of the North China Craton and its bearing on tectonic setting. International Geology Review 40, 706–21.CrossRefGoogle Scholar
Zhao, G. C., Wilde, S. A., Cawood, P. A. & Lu, L. Z. 2000 b. Petrology and P–T path of the Fuping mafic granulites: implications for tectonic evolution of the central zone of the North China craton. Journal of Metamorphic Geology 18, 375–91.CrossRefGoogle Scholar
Zhao, G. C., Wilde, S. A., Cawood, P. A. & Sun, M. 2001 b. Archean blocks and their boundaries in the North China Craton: lithological, geochemical, structural and P–T path constraints and tectonic evolution. Precambrian Research 107, 45–73.CrossRefGoogle Scholar
Zhao, G. C., Wilde, S. A., Cawood, P. A. & Sun, M. 2002. SHRIMP U–Pb zircon ages of the Fuping Complex: implications for Late Archean to Paleoproterozoic accretion and assembly of the North China Craton. American Journal of Science 302, 191–226.CrossRefGoogle Scholar
Zhao, G. C., Wilde, S. A., Guo, J., Cawood, P. A., Sun, M. & Li, X. P. 2010. Single zircon grains record two Paleoproterozoic collisional events in the North China Craton. Precambrian Research 177, 266–76.CrossRefGoogle Scholar
Zhao, G. C., Wilde, S. A., Sun, M., Li, S. Z., Li, X. P. & Zhang, J. 2008. 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 Research 160, 213–26.CrossRefGoogle Scholar
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