Abstract
Whether or not Grenvillian orogeny occurred in South China still remains highly controversial because high-quality, discriminating data are lacking, and therefore, the key to resolve this matter is to find datable volcanic and/or sedimentary rocks related to Grenvillian orogeny. Such rocks are apparently present in the Fuliangpeng Member from the lower-middle part of Kunyang Group in central Yunnan; here the unit is more than 100 m thick and consists of andesitic ignimbrite, tuffite, terrigeous clastic rocks and carbonates. These volcanic rocks, developed south of the Sibao fold-thrust belts, represent the earliest calc-alkaline volcanic activity in late Precambrian time from central Yunnan and are coeval with both a change in sedimentary facies from detritus to carbonates and the beginning of seismite development elsewhere. Two samples for SHRIMP analysis were collected from this volcanic unit. Sample G3-29-2, from the bottom of Fuliangpeng Member, is an ignimbrite, and about 100 zircon crystals recovered from it have euhedral shapes and display relatively simple sector zonation under cathodoluminescent (CL) imaging, suggesting a magmatogenic origin. Twenty-five of the zircons were analyzed and a weighed-mean U-Pb age of 1032±9 Ma was obtained. Sample G3-29-3 from uppermost part of Fuliangpeng Member is a tuffite, and many rounded, evidently detrital zircons were recovered. Nine of these zircons were analyzed, and the oldest single-grain U-Pb zircon age is 1938±26 Ma, implying that Paleoproterozoic basement developed in Cathaysia. The dating result, combined with the geotectonic research on the Fuliangpeng Member, leads us to conclude that late Mesoproterozoic orogenic volcanic activity occurred in the western part of South China, and that the related collision of Yangtze and Cathaysian cratons was an integral part of the assembly of Rodinia.
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References
Davidson J S. New interpretation of the southwestern Grenville province. In: Moores J M Jr, Davidson A, Baer A J, eds. The Grenville Province. Geological Association of Canada Special Paper 31, 1986. 61–74
Moores E M. Southwest U.S.-East Antarctic (SWEAT) connection: A hypothesis. Geology, 1991, 19(5): 425–428
Rainbird R H, Heaman L M, Young G M. Sampling Laurentia: detrital zircon geochronology offers evidence for an extensive Neoproterozoic river system originating from Grenville orogen. Geology, 1992, 18(4): 100–108
Heizler M T Ralser S, Karlstrom K E. Late Proterozoic (Grenville?) deformation in central New Mexico determined from single-crystal muscovite 40Ar/39Ar age spectra. Precambrian Res, 1997, 84: 1–15
Karlstrom K E, Ahall K-I, Harlan S S, et al. Long-lived (1.8–1.0Ga) convergent orogen in southern Laurentia, its extensions to Australia and Baltica, and implications for refining Rodinia. Precambrian Res, 2001, 111: 5–30
Fitzsimons I C W. Grenville-age basement provinces in East Antarctica: Evidence for three separate collisional orogens. Geology, 2000, 28(10): 879–882
Jacobs J, Falter M, Thomas R J, et al. 40Ar/39Ar Thermochronological constraints on the structural evolution of the Mesoproterozoic Natal Metamorphic Province, SE Africa. Precambrian Res, 1997, 86:71–92
Spikings R A, Foster D A, Kohn B P, et al. Post-orogenic (<1500 Ma) thermal history of the Palaeo-Mesoproterozoic, Mt. Isa province, NE Australia. Tectonophysics, 2002, 349: 327–365
Li Z X, Zhang L H, Powell C McA. South China in Rodinia: Part of the missing link between Australia-East Antarctica and Laurentia? Geology, 1995, 23(5): 407–410
Zhang L H, Li Z X, Powell C McA. Correlation of the Neoproterozoic sequences between the Yangtzean and the Australia Paleocontinents and a paleocontinental reconstruction. Earth Sci-J China Univ Geosci (in Chinese), 1994, 20(6): 657–667
Li Z X, Powell C McA. Break of Rodinia and Gondwanaland and assembly of Asia. Australian J Earth Sci, 1996, 43(4): 591–592
Zhou M F, Yan D P, Kennedy A K, et al. SHRIMP U-Pb zircon geochronological and geochemical evidence for Neoproterozoic arc-magmatism along the western margin of the Yangtze Block, South China. Earth Planet Sci Lett, 2002, 196: 51–67
Li Z X, Li X H, Zhou H W, et al. Grenvillian continental collision in south China: New SHRIMP U-Pb zircon results and implications for the configuration of Rodinia. Geology, 2002, 30(2): 163–166
Yan D P, Zhou M F, Song H L, et al. Where was South China located in the reconstruction of Rodinia? Earth Sci Front (in Chinese), 2002, 9(4): 249–256
Li X H. U-Pb zircon ages of granites from the southern margin of the Yangtze Block: timing of Neoproterozoic Jinning: Orogeny in SE China and implications for Rodinia Assembly. Precambrian Res, 1999, 97:43–57
Li Z X, Li X H, Kinny P D, et al. The breakup of Rodinia: Did it start with a mantle plume beneath South China? Earth Planet Sci Lett, 1999, 173: 171–181
Li X H, Li Z X, Zhou H W, et al. SHRIMP U-Pb zircon age, geochemistry and Nd isotope of the Guandaoshan pluton in SW Sichuan: Petrogenesis and tectonic significance. Sci China Ser D-Earth Sci, 2003, 46(Suppl): 73–83
Li X H, Li Z X, Ge W C, et al. Neoproterozoic granitoids in South China: crustal melting above a mantle plume at ca. 825 Ma? Precambrian Res, 2003, 122: 45–83
Wu M D, Duan J S, Song X L, et al. Geology of Kunyang Group in Yunnan (in Chinese). Kunming: Yunnan Science and Technology Publishing House, 1990. 1–265
Li X J, Wu M D, Duan J S. The stratigraphic sequence of the Kunyang Group and its top and bottom boundaries. Geol Rev (in Chinese), 1984, 30(5): 399–408
Li F H, Wang F X, Shen Y L, et al. The Pre-Cambrian in West Sichuan and Yunnan (in Chinese). Chongqing: Chongqing Publishing House, 1988. 1–214
Dai H G. On the strata, structure and prospecting target area of Kunyang Group and Huili Group in Kang-Dian region. Yunnan Geol (in Chinese), 1997, 16(1): 1–39
Lu S K, Dai H G. A review of the set-up of Kunyang Group’s sequence and the discovery of important ore-bearing horizons in Kang-Dian area. Yunnan Geol (in Chinese), 2001, 20(1): 1–24
Liu D Y, Jian P, Zhang Q, et al. SHRIMP dating of adakites in the Tulingkai ophiolite, Inner Mongolia: evidence for the early Paleozoic subduction. Acta Geot Sin, 2003, 77(3): 317–327
Jian P, Liu D Y, Zhang Q et al. SHRIMP dating of ophiolite and leucocratic rocks within ophiolite, Earth Sci Front (in Chinese), 2003, 10(4): 439–456
Du Y S, Zhang C H, Han X et al. Earthquake event deposits in Mesoproterozoic Kunyang Group in central Yunnan and its geological implications. Sci China Ser D-Earth Sci, 2001, 44(7): 600–608
Gill J B. Orogenic Andesites and Plate Tectonics. Berlin: Springer-Verlag, 1981. 1–90
Mou C L, Lin S L, Yu Q. Sedimentation and evolution of the Mesoproterozoic Kunyang Group in the Huili-Huidong region, Sichuan and its adjacent areas. Sediment Geol Tethyan Geol (in Chinese), 2000, 20(1): 44–51
Zhou C X, Wei C S, Li C Y. Lower Sinian igneous rock suits along the southwestern margin of the Yangtze block. Acta Miner Sin (in Chinese), 1998, 18(4): 405–410
Sun C M. Proterozoic ophiolites in western Sichuan and the Proterozoic orogenic belt on the west border of Yangtze paleo-plate. J Chengdu Institute Tech (in Chinese), 1994, 21(4): 11–16
Du Y S, Han X. Preliminary notes on evolution and dynamics of the Proterozoic sedimentary basins of central Yunnan. Geoscience—J Graduate School of China Univ Geosci (in Chinese), 1999, 13(2):232–234
Mosher S. Tectonic evolution of the southern Laurentian Grenville orogenic belt. GSA Bull, 1998, 110(11): 1357–1375
Grew E S, Manton W I. A new correlation of sapphirine granulites in the Indo-Antarctic metamorphic terrain, late Proterozoic dates from the Eastern Ghats Province of India. Precambrian Res, 1986, 33:123–137
Katz M B. Sri Lanka-Indian eastern Ghats-east Antatctica and the Australian Albany Fraser mobile belt, Gross geometry, age relationships, and tectonics in Precambrian Gondwanaland. J Geol, 1989, 97:646–648
Boger S D, Carson C J, Wilson C J L, et al. Neoproterozoic deformation in the Radok Lake region of the northern Prince Charles Mountains, east Antarctica; evidence for a single protracted orogenic event. Precambrian Res, 2000, 104: 1–24
Pidgeon R T. Timing of plutonism in the Proterozoic Albany mobile belt, southwestern Australia. Precambrian Res, 1990, 47: 157–167
Greentree M R, Li Z X, Li X H, et al. Late Mesoproterozoic to earliest Neoproterozoic basin record of the Sibao orogenesis in western South China and relationship to the assembly of Rodinia. Precambrian Res, 2006, 151: 79–100
Li X H, Li Z X, Sinclair J A et al. Revisiting the “Yanbian Terrane”: implications for Neoproterozoic tectonic evolution of the western Yangtze Block, South China. Precambrian Res, 2006, 151: 14–30
Deng S X, Wang J H, Zhu B Q. P-T-t path of metamorphism for the Julin Group and its geodynamical implications in Yuanmou, Yunnan. Sci China Ser D-Earth Sci, 2001, 44(7): 609–620
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Supported by China Geological Survey (Grant No. 200313000055), Program for Changjiang Scholars and Innovative Research Team in University (Grant No. IRT0546) and the National Natural Science Foundation of China (Grant No. 40621002)
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Zhang, C., Gao, L., Wu, Z. et al. SHRIMP U-Pb zircon age of tuff from the Kunyang Group in central Yunnan: Evidence for Grenvillian orogeny in South China. CHINESE SCI BULL 52, 1517–1525 (2007). https://doi.org/10.1007/s11434-007-0225-x
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DOI: https://doi.org/10.1007/s11434-007-0225-x