[an error occurred while processing this directive] Global Geology 2018, 21(1) 14-25 DOI:   10.3969/j.issn.1673-9736.2018.01.02  ISSN: 1673-9736 CN: 22-1371/P

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Baicaogou tuff
zircon U-Pb age
I-type granite
subduction
Paleo-Pacific
Yanji
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PubMed
Geochronology and geochemistry of Baicaogou tuff in Yanji, NE China and its tectonic implications for Early Cretaceous
WANG Yingchao, SUN Fengyue, LI Liang, XIN Wei, YAN Jiaming, TIAN Lidan
College of Earth Sciences, Jilin University, Changchun 130061, China
ժҪ�� The authors studied zircon U-Pb age and geochemical data of Baicaogou tuff in Yanji, Jilin Province. The results indicate that the rocks formed in Early Cretaceous (125. 6±2. 3 Ma). Geochemically, these tuffs have high SiO2 and total Na2O + K2O, low MgO and FeO, and they belong to metaluminous series, the rock are enriched in LREEs and LILEs, depleted in HREEs and HFSEs such as Nb, Ta, Ti, and P, exhibiting an affinity to I-type granite. All these characteristics implied that the volcanic rocks were derived from partial melting of lower crust. Combined with the geochronology and geochemical features of the coeval igneous rocks within NE China, it is concluded that Yanji area was in a back-arc extensional setting in response to the subduction of the Paleo-Pacific Plate beneath the Eurasian Plate.
�ؼ����� Baicaogou tuff   zircon U-Pb age   I-type granite   subduction   Paleo-Pacific   Yanji  
Geochronology and geochemistry of Baicaogou tuff in Yanji, NE China and its tectonic implications for Early Cretaceous
WANG Yingchao, SUN Fengyue, LI Liang, XIN Wei, YAN Jiaming, TIAN Lidan
College of Earth Sciences, Jilin University, Changchun 130061, China
Abstract: The authors studied zircon U-Pb age and geochemical data of Baicaogou tuff in Yanji, Jilin Province. The results indicate that the rocks formed in Early Cretaceous (125. 6±2. 3 Ma). Geochemically, these tuffs have high SiO2 and total Na2O + K2O, low MgO and FeO, and they belong to metaluminous series, the rock are enriched in LREEs and LILEs, depleted in HREEs and HFSEs such as Nb, Ta, Ti, and P, exhibiting an affinity to I-type granite. All these characteristics implied that the volcanic rocks were derived from partial melting of lower crust. Combined with the geochronology and geochemical features of the coeval igneous rocks within NE China, it is concluded that Yanji area was in a back-arc extensional setting in response to the subduction of the Paleo-Pacific Plate beneath the Eurasian Plate.
Keywords: Baicaogou tuff   zircon U-Pb age   I-type granite   subduction   Paleo-Pacific   Yanji  
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DOI: 10.3969/j.issn.1673-9736.2018.01.02
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Anderson T. 2002. Correction of common lead in U-Pb analyses that donot report 204 Pb.Chemical Geology,192(1):59-79.
Annen C, Blundy J D, Sparks R S J. 2006.The genesis of intermediate and silicic magmas in deep crustal hot zones.Journal of Petrology,47(3):505-539.
Belousova E A, Griffin W L, O'Reilly S Y, et al. Igneous zircon:trace element composition as an indicatorof source rock type.Contributions to Mineralogy and Petrology, 2002,143(5):602-622.
Chen B, Jahn B M, Wilde S,et al. 2000. Two contrasting Paleozoic magmatic belts in northern Inner Mongolia, China:petrogenesis and tectonic implications.Tectonophysics,328:157-182
Chen B, Jahn B M, Tian W. 2009. Evolution of the Solonker suture zone:constraints from zircon U-Pb ages, Hf isotopic ratios and whole-rock Nd-Sr isotope compositions of subduction and collision-related magmas and forearc sediments.Journal Of Asian Earth Sciences,34:245-257
Chappell B W, 1999. Aluminium saturation in I-type and S-type granites and the characterization of fractionated haplogranites.Lithos,46(9):535-551.
Dewey J F. 1988. Extensional collapse of orogens.Tectonics,7:1123-1139.
Fan W M,Guo F,Wang YJ,et al. 2003. Late Mesozoic calcalkaline volcanism of post-orogenic extension in the northern Da Hinggan Mountains, northeastern China.Journal of Volcanology and Geothermal Research,121(1):115-135.
Gil F, Pla A. 2001.Biomarkers as biological indicators of xenobiotic exposure.Toxicology science,21:245-255,
Ge W C,Lin Q, Sun D Y, et al. 2000. Geochemical research into origin of two types of Mesozoic rhyolites in Daxing'anling.Earth Science,25(2):172-178. (in Chinese with English abstract)
Ge R F, Zhang Q L, Wang L S,et al. 2012. Late Mesozoic rift evolution and crustal extension in the central Songliao Basin, northeastern China:constraints from cross-section restoration and implications for lithospheric thinning Int.Geology Research,54:183-207.
Ge W C, Wu F Y, Zhou C Y,et al, 2005. Zircon U-Pb ages and its significance of the Mesozoic granites in the Wulanhaote region, central Da Hinggan Mountain.Acta Petrol Sin,21:749-762. (in Chinese with English abstract)
Han B, Wang S, Jahn B,et al. 1997. Depleted-mantle sourcefor the Ulungur River A-type granites from North Xinjiang,China:geochemistry and Nd-Sr isotopic evidence,and implications for Phanerozoic crustal growth.Chemical Geology,138(3):135-159.
Hildreth W, Moorbath S. 1988. Crustal contributions to arcmagmatism in the Andes of central Chile.Contributions to Mineralogy and Petrology,98(4):455-489.
Jahn B M, Wu F Y, Chen B. 2000.Massive granitoid generation in Central Asia:Nd isotope evidence and implication for continental growth in the Phanerozoic.Episodes,23:82-92.
Jahn B M R, Capdevila D Y, Liu A,et al. 2004.Sources of Phanerozoic granitoids in the transect Bayanhongor-Ulaan Baatar, Mongolia:geochemical and Nd isotopic evidence, and implications for Phanerozoic crustal growth.Journal Of Asian Earth Sciences,23:629-653.
Jahn B.M, Wu F Y, Capdevila R,et al. 2001. Highly evolved juvenile granites with tetrad REE patterns:the Woduhe and Baerzhe granites from the Great Xing'an Mountain in NE China.Lithos,59:171-198.
Jahn B M, Litvinovsky B A, Zanvilevich A N, et al. 2009. Peralkaline granitoid magmatism in the Mongolian-Transbaikalian belt:evolution, petrogenesis and tectonic significance.Lithos,113:521-539.
Jilin Bureau of Geology and Mineral Resources (JBGMR). 1988. Regional geology of Jilin Province. Beijing:Geological Publishing House, 1-670. (in Chinese with English abstract)
Kravchinsky V A, Cogné J P, Harbert W P, et al. 2002. Evolution of the Mongol-Okhotsk Ocean as constrained by new palaeomagnetic data from the Mongol-Okhotsk suture zone,Siberia Geophys,148:34-57.
Lehmann J, Schulmann K, Lexa O,et al. 2010. Structural constraints on the evolution of the Central Asian orogenic belt in SW Mongolia.Life Sciences,310:575-628.
Lin Q, Ge W C, Sun Y,et al. 1998. Tectonic significance of Mesozoic volcanic rocks in Northeast China. Geological Science,18(2):3-13.
Liu Y, Hu Z, Gao S,et al. 2008. In situ analysis of majorand trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard.Chemical Geology,257(1):34-43.
Ludwig K R. 2003. User's manual for Isoplot:a geochronological tool kit for Microsoft Execl. Berkeley:Berkeley Geochronology Center Special Publication, 4-1-70.
Lin Q, Ge W C, Sun D Y,et al. 1998. Tectonic significance of Mesozoic volcanic rocks in northeastern China.Scientia Geological Sinica,33(2):129-139.(in Chinese with English abstract)
Liu S, Hu R Z, Gao S,et al. 2010. Zircon U-Pb age and Sr-Nd-Hf isotope geochemistry of Permian granodiorite and associated gabbro in the Songliao Block, NE China and implications for growth of juvenile crust.Lithos,114:423-436.
Middlemost E A K. 1972. A simple classification of volcanic rocks. Bulletin Volcanologique,36:382-397
Meng Q L, Zhou Y C, Chai S L. 2001. Porphyry hydrothermal vein type Cu-Au deposits, eastern Yanbian. Changchun:Jilin Science Technology Press, 1-163. (in Chinese)
Maniar P D, Piccoli P M. 1989. Tectonic discrimination of granitoids.Geological Society of America Bulletin,101:635-643.
Maruyama S, Isozaki Y, Kimura G,et al.1997. Paleogeographic maps of the Japanese Islands:plate tectonic synthesis from 750 Ma to the present. Island Arc,6:121-142.
Ma X H, Chen B, Yang M C.2013. Magma mixing origin for the Aolunhua porphyry related to Mo-Cu mineralization, eastern Central Asian Orogenic Belt.Gondwana Research,24:1152-1171.
Ma X H, Cao R, Zhou Z H,et al. 2015. Early Cretaceous high-Mg diorites in the Yanji area, northeasternChina:Petrogenesis and tectonic implications.Journal of Asian Earth Sciences,97:393-405.
Peccerillo A, Taylor S R, 1976. Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area.Contributions to Mineralogy & Petrology,58(1):63-81.
Rudnick R L, Cao S. 2003. Composition of the continental crust//Rudnick R L.(ed.) The crust treaties on geochemistry. Oxford:Elsevier Pergamon, 1-64.
Ruzhentsev S V, Pospelov I I. 1992. The south Mongolian Variscan fold system.Geotectonics,26:383-395.
Sorokin A, Kotov A, Sal'nikova E B, et al. 2010. Ranitoids of the Tyrma-Bureya complex in the northern Bureya-Jiamusi superterrane of the Central Asian fold belt:age and geodynamic setting.Russian Geology and Geophysics,51(5):563-571.
Sun S S, McDonough W F. 1989. Chemical and isotopic systematics of oceanic basalts:implition for mantle composition and processes.Geoligical Socity Special Publication,42(1):313-345.
Turner S P, Foden J D, Morrison R S. 1992. Derivation of some A-type magmas by fractionation of basaltic magma:an example from the Padthaway Ridge, South Australia.Lithos, 28(2):151-179.
Tatsumi Y, Kimura N, 1991. Backarc extension versus continental breakup:petrological aspects for active rifting.Tectonophysics,197:127-137.
Wu F Y, Yang J H, Lo C H,et al. 2007. The Heilongjiang Group:a Jurassic accretionary complex in the Jiamusi Massif at the western Pacific margin of northeastern China.The Island Arc,16:156-172.
Wu F Y, Jahn B M, Wilde S,et al. 2000. Phanerozoic crustal growth:U-Pb and Sr-Nd isotopic evidence from the granites in northeastern China.Tectonophysics,328:89-113.
Wu F Y, Lin J Q, Wilde S A,et al. 2005. Nature and significance of the Early Cretaceous giant igneous event in eastern China Earth Planet. Earth Planetary Science Letters,233:103-119.
Wu F Y, Sun D Y, Ge W C,et al.2011.Geochronology of the Phanerozoic granitoids in northeastern China.Journal of Asian Earth Sciences,41:1-30.
Wu F Y, Sun D Y, Li H M,et al. 2002. A-type granites in northeastern China:age and geochemical constraints on their petrogenesis. Chemical Geology,187:143-173.
Windley B F, Alexeiev D, Xiao W,et al. 2007. Tectonic models for accretion of the Central Asian Orogenic Belt. Geological Societey,164(12):31-47.
Weaver B L. 1991.The origin of ocean island basalt end-member compositions:trace element and isotopic constraints.Earth Planetary Science Letter,104:381-397.
Wickham S M, Litvinovsky B A, Zanvilevich A N,et al.1995. Geochemical evolution of Phanerozoic magmatism in Transbaikalia, East Asia:a key constraint on the origin of K-rich silicic magmas and the process of cratonization. Geophysics Research,100:15641-15654.
Xu B, Charvet J, Chen Y,et al. 2013. Middle Paleozoic convergent orogenic belts in western Inner Mongolia(China):framework, kinematics, geochronology and implications for tectonic evolution of the Central Asian Orogenic Belt.Gondwana Research,23(4):1342-1364.
Yang J H, Wu F Y,Chung S L,et al. 2006. A hybrid originfor the Qianshan A-type granite, northeast China:geochemical and Sr-Nd-Hf isotopic evidence. Lithos,89(1):89-106.
Yuan H L,Gao S,Liu X M,et al. 2004.Accurate U-Pb age and trace element determinations of zircon by laser ablationinductively coupled plasma-mass spectrometry.Geostandards and Geoanalytical Research,28(3):353-370.
Yuan H L, Wu F Y, Gao S,et al. 2003. Zircon from Cenozoic intrusive body laser probe U-Pb time dating and rareearth element composition analysis.Chinese Science Bulletin,48(14):1511-1520. (in Chinese with English abstract)
Zhao Y, Yang Z Y, Ma X H. 1994. Geotectonic transition from Paleo-Asian system and Paleo-Tethyan system to Paleo-Pacific active continental margin in eastern Asia.Scientia Geological Sinica,29:105-119.(in Chinese with English abstract)
Zhang Y B. 2002. The isotopic geochronoligic frame of granitic magmatism in Yanbian area:doctor's degree thesis. Changchun:Jilin University. (in Chinese with English abstract)
Zhao H L, Deng J F, Chen F J,et al. 1998.Petrology of the Mesozoic volcanic rocks and the basin formation in the Northeast China.Geoscience,12(1):56-62. (in Chinese with English abstract)
Zhou J B, Wilde S A, Zhang X Z,et al. 2009. The onset of Pacific margin accretion in NE China:evidence from the Heilongjiang high-pressure metamorphic belt.Tectonophysics,478:230-246.
Zhang J H, Ge W C, Wu F Y,et al. 2008. Large-scale Early Cretaceous volcanic events in the northern GreatXing' an Range, Northeastern China.Lithos,102(1/2):138-157.
Zonenshain L P, Kuzmin M I, Natapov L M. 1990. Geology of the USSR:a plate-tectonic synthesis. Washing D.C.:American Geophysical Union, 1-242
Zhang F Q, Chen H L, Yu X,et al. 2011. Early Cretaceous volcanism in the northern Songliao Basin, NE China, and its geodynamic implication.Gondwana Research,19:163-176.
Zhang L C, Ying J F, Chen Z G,et al. 2008. Age and tectonic setting of Triassic basic volcanic rocks in southern Da Hinggan Range.Acta Petrologica Sinica,24:911-920.(in Chinese with English abstract)
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