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Article by Du C
Article by Liu Z
Article by Li P
Article by Guan Q
Article by Chen X
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1. ���ִ�ѧ�����ѧѧԺ, ���� 130061;
2. �˹�ҵ���������, ���ɹų�� 024000
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LA-ICP-MS zircon U-Pb dating, geochemical characteristics and geological significance of tonalitic gneisses from Banshigou area of southern Jilin
DU Chuan-ye1, LIU Zheng-hong1, LI Peng-chuan1, GUAN Qing-bin1, CHEN Xu2
1. College of Earth Sciences, Jilin University, Changchun 130061, China;
2. No. 243 Geological Party of Nuclear Industry, CNNC, Chifeng 024000, Inner Mongolia, China
Abstract: The authors discusse the origin and evolution mechanism of tonalitic gneisses from Banshigou area of southern Jilin. It is indicated that the TTG gneisses are characterized by high Si(SiO2=66.61%~72.35%), Al(Al2O3=13.56%~16.18%) and Na(Na2O=3.65%~4.69%), but low K(K2O=1.13%~2.25%). The chondrite normalized REE patterns are characterized by right inclining type. Trace element analysis shows the enrichment of large ion lithophile elements (e.g., Ba and Rb) and strong depletion in high field strength elements (e.g., Ni and Ta).The gneisses belong to the high aluminum TTG gneisses with geochemical characteristics similar to the high silicon adakite. LA-ICP-MS zircon U-Pb age data indicate that the rocks were crystallized at (2 619±28)Ma, so they are formed in Neoarchean. Zircon Lu-Hf isotopic analyses show that the magma is rarely mixed with the mantle material during its evolution, and the corresponding two-stage model age(TDM2) is mainly between 2 976 Ma and 2 675 Ma.Therefore, tonalitic gneisses of Banshigou area are probably produced by partial melting of basaltic oceanic crust in the subduction environment. The authors suggest that there probably existed an orogenic belt (Ji-Liao-Ji arc-continent collision orogenic belt) in Neoarchean in the northeast North China Craton.
Keywords: southern Jilin   Banshigou area   TTG gneisses   Neoarchean   zircon U-Pb age   oceanic crust  
�ո����� 2017-05-05 �޻����� 2017-07-08 ����淢������  
DOI: 10.3969/j.issn.1004-5589.2017.03.009
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[1] Liu D Y,Nutman A P,Compston W,et al.Remnants of �� 3800 Ma crust in the Chinese part of the Sino-Korean Craton[J].Geology,1992,20(4):339-342.
[2] Rogers J J W,Santosh M.Supercontinents in Earth history[J].Gondwana Research,2003,6(3):357-368.
[3] Zhai M G,Guo J H,Liu W J.Neoarchean to Paleoproterozoic continental evolution and tectonic history of the North China Craton:a review[J].Journal of Asian Earth Sciences,2005,24(5):547-561.
[4] ������,����һ,������,��.�й�������ʯ���ʯ[J].��ʯѧ��,2009,25(8):1793-1807. WAN Yu-sheng,LIU Dun-yi,DONG Chun-yan,et al.The oldest rocks and zicrons in China[J].Acta Petrologica Sinica,2009,25(8):1793-1807.
[5] ������.��������ͨ���γ��ݻ���ɿ�����[J].�󴲵���,2010,29(1):24-36. ZHAI Ming-guo.Tectonic evolution and metallogenesis of North China Craton[J].Mineral Deposits,2010,29(1):24-36.
[6] Condie K C.TTGs and adakites:are they both slab melts[J]. Lithos,2005,80(1/4):33-44.
[7] ����Ӣ,�ų���,����.��������ͨ~2.5 Ga�ؿ������¼�:��������ɽTTG��Ƭ���ҵ�֤��[J].��ʯѧ��,2013,29(7):2265-2280. ZHANG Rui-ying,ZHANG Cheng-li,SUN Yong.Crustal reworking in the North China Craton at~2.5 Ga:evidence from zircon U-Pb ages,Hf isotopes and whole-rock geochemistry of the TTG gneisses in the Zhongtiao Mountain[J]. Acta Petrologica Sinica,2013,29(7):2265-2280.
[8] ����ˬ,������,������,��.����ɽ�ˮ������TTGƬ���ҵ��ʯHfͬλ�����������γɻ���[J].��ʯѧ��,2008,24(1):139-148. GUO Li-shuang,LIU Shu-wen,LIU Yu-lin,et al.Zircon Hf isotopic features of TTG gneisses and formation environment of Prceambrian Sushui complex in Zhongitao Mounatin[J].Acta Petrologica Sinica,2008,24(1):139-148.
[9] ����,������,·Тƽ.��������ͨ2.5 Ga�ؿ������¼���Nd-Hfͬλ��֤��:�Ի���Ƭ���ҵ���Ϊ��[J].��ѧͨ��,2009,54(17):2517-2526. LIU Fu,GUO Jing-hui,LU Xiao-ping.Crustal growth at~2.5 Ga in the North China Craton:evidence from whole-rock Nd and zircon Hf isotopes in the Huai'an gneisses terrane[J]. Chinese Science Bulletin,2009,54(17):2517-2526.
[10] ·����,�λ���,������,��.��������ͨ��ƽ������~2.7 Ga TTGƬ���ҵ��嶨�����������[J].��ʯѧ��,2014,30(10):2872-2884. LU Zeng-long,SONG Hui-xia,DU Li-lin,et al. Delineation of the ca. 2.7 Ga TTG gneisses in the Fuping Complex,North China Craton and its geological significance[J].Acta Petrologica Sinica,2014,30(10):2872-2884.
[11] ������,������,��ƽ��,��.������ǰ����ͱ��ʻ��׶����ҽ�-�������¼�:����TTGƬ���Һͻ�����Ƭ�������ʯU-Pb�����֤��[J].��ʯѧ��,2011,27(4):943-960. LIU Jian-hui,LIU Fu-lai,LIU Ping-hua,et al.Polyphase magmatic and metamorphic events from Early Precambrian metamorphic basement in Jiaobei area:evidences from the zircon U-Pb dating of TTG and granitic gneisses[J].Acta Petrologica Sinica,2011,27(4):943-960.
[12] ������,��̫ƽ,Ѧ��ΰ,��.������ɽ������̫�Ŵ�TTG��Ƭ���ҵij������������:������ʯѧ������ѧ��ͬλ�����ѧ����Լ[J].��ʯѧ��,2009,25(2):331-347. ZHOU Yan-yan,ZHAO Tai-ping,XUE Liang-wei,et al.Petrological,geochemical and chronologlcia cosntriants for the origan and geological significance of Neoarchean TTG gneisses in the Songshan area,North China Craton[J].Acta Petrologica Sinica,2009,25(2):331-347.
[13] ����,���ǿ,������,��.³��2.5~2.7 Ga�����ҽ����¼�:̩ɽ��ǰˮ��TTG�����ҵ�Ұ����ʺ��ʯSHRIMP����[J].��������,2015,61(5):1068-1078. REN Peng,XIE Hang-qiang,WANG Shi-jin,et al.2.5~2.7 Ga tectono-thermal events in western Shandong:geology and zircon SHRIMP dating of TTG rocks in Huangqian reservior,Taishan Mountain[J].Geological Review,2015,61(5):1068-1078.
[14] ½����,��־��,����Ⱥ.̩ɽ������ʹ�԰����������ϵ������[M].����:���ʳ�����,2008:1-78. LU Song-nian,CHEN Zhi-hong,XIANG Zhen-qun.Geochronology framework of the oldest intrusive complex in Taishan geological park,Shandong Province[M]. Beijing:Geological Publishing House, 2008:1-78.
[15] ������,�Ž���,��ʤҢ,��.�������Ƶؿ�~2.5 Ga TTG��ʯ����������[J].��ѧͨ��,2012,57(28/29):2715-2728. GONG Jiang-hua, ZHANG Jian-xin, YU Sheng-yao,et al.2.5 Ga TTG rocks in the western Alxa Block and their implications[J].Chinese Science Bulletin,2012,57(28/29):2715-2728.
[16] ������,����Ԫ,������,��.���ɹ��в����������˵���̫����߼��������ʯU-Pb���ѧ�о�[J].�й���ѧ:�����ѧ,2012,42(7):1001-1010. DONG Xiao-jie,XU Zhong-yuan,LIU Zheng-hong,et al.Zircon U-Pb geochronology of Archean high-grade metamorphic rocks from Xi Wulanbulang area,central Inner Mongolia[J].Science in China:Earth Science,2012,42(7):1001-1010.
[17] ������,����Ԫ,������,��.���ɹ��䴨���������˵�����ǰ����ͱ��ʻ����ʯSHRIMP���꼰Hfͬλ�����[J].��ʯѧ��,2013,29(2):501-516. MA Ming-zhu,XU Zhong-yuan,ZHANG Lian-chang,et al.SHRIMP dating and Hf isotope analysis of zircons from the Early Precambrian basement in the Xi Ulanbulang area,Wuchuan,Inner Mongolia[J]. Acta Petrologica Sinica,2013,29(2):501-516.
[18] Kröner A,Wilde S A,Li J H,Wang K Y.Age and evolution of a Late Archean to Paleoproterozoic upper to lower crustal section in the Wutaishan-Hengshan-Fuping terrain of northern China[J].Journal of Asian Earth Sciences,2005,24(5):577-595.
[19] Faure M,Trap P,Lin W,et al.Polyorogenic evolution of the Paleoproterozoic trans-north China belt:new in sights from the Lüliangshan-Hengshan-Wutaishan and Fuping massifs[J].Episodes,2007,30(2):96-107.
[20] Yang C H,Du L L,Ren L D,et al.Delineation of the ca.2.7 Ga TTG gneisses in the Zanhuang complex,North China Craton and its geological implications[J].Journal of Asian Earth Sciences,2013,72:178-189.
[21] �,����ҵ,�ŵ,��.����ʡ��ʯ��)-���Ĵ����Ҵ���ʯ����ѧ���������һ�������[J].���ֵ���, 1993,12(3):24-31. YANG Bao,BI Shou-ye,ZHANG Dan-fa,et al.Geological characteristics of the Banshigou-Wangwenchuan greenstone belt and the diagenetic analysis in Jilin Province[J]. Jilin Geology, 1993,12(3):24-31.
[22] ��־��,����ʥ.���ϴ�Ĺ�-��ʯ��������ǰ����ͱ��ʱ������ü��ؿ��ݻ�[J].�й��������, 1995,14(3):228-232. LIU Zhi-hong,JIANG Ji-sheng.Early Precambrian metamorphism, deformation and crustal evolution in the Dahuangou-Banshigou area, southern Jilin[J]. Regional Geology of China, 1995,14(3):228-232.
[23] ��־��,����ʥ,������.�����ϲ���ʯ�����������Ͽ��ҵ�Sm-Ndͬλ�����估���������[J].��ʯ����ѧ��־, 1999,18(1):46-49. LIU Zhi-hong,JIANG Ji-sheng,YANG Zhen-sheng.Sm-Nd ages of the metasupercrustal rocks in Banshigou area of southern Jilin and their implications[J]. Acta Petrologica et Mineralogica, 1999,18(1):46-49.
[24] ����ʵ,������,������,��.���ϰ�ʯ������ǰ����͹����ͱ����м��ؿ��ݻ�[J].�й��������, 1999,18(4):383-390. SUN Zhong-shi, FENG Ya-min, YANG Xiao-dong,et al.The Precambrian ductile deformation sequence and crustal evolution in Banshigou, South Jilin[J]. Regional Geology of China, 1999,18(4):383-390.
[25] ����ʵ,�˾�,������.�����ϲ�������̫����-Ԫ����ֽ�ʱ�޵�ȷ���������Թ����ݻ�[J].��������,2000,46(2):197-202. SUN Zhong-shi,DENG Jun,LIU Ya-qin.Determination of Archaean-Proterozoic boundry for the metamorphic rocks and the transitional tectonic evolution in southern Jilin[J].Geological Review,2000,46(2):197-202.
[26] ������,�ű���,������.����ʡ��ʯ�����������������[J].���ֵ���, 1992,11(3):1-10. QU Fen-xiong, ZHANG Bao-hua,CUI Wen-zhi.The geological features of the Banshigou iron mining, Jilin Province[J]. Jilin Geology, 1992,11(3):1-10.
[27] ������,�ű���,������.�����û�����ؿ����:�Լ��ְ�ʯ������Ϊ��[J].���ʿ�ѧ,1997,32(1):103-109. QU Fen-xiong,ZHANG Bao-hua,LIU Ru-qi.Structural transposition and its controlling effect on iron deposits:an example from Banshigou iron deposit, Jilin Province, China[J]. Scientia Geologica Sinica,1997,32(1):103-109.
[28] Zhao G C,Cawood P A,Wilde S A,et al.Metamorphism of basement rocks in the central zone of the North China Craton:implications for Palaeoproterozoic tectonic evolution[J].Precambrian Research,2000,103(1/2):55-88.
[29] Zhao G C,Sun M,Wilde S A,et al.Late Archean to Paleoproterozoic evolution of the North China Craton:key issues revisited[J]. Precambrian Research,2005,136(2):177-202.
[30] ������,������,���ǿ,��.��������ͨ��ǰ���������״�������γ�ʱ��:SHRIMP�ʯU-Pb����[J]. ����ѧ��, 2012,86(9):1447-1478. WAN Yu-sheng,DONG Chun-yan,XIE Hang-qiang,et al.Formation ages of Early Precambrian BIFs in the North China Craton:SHRIMP zircon U-Pb dating[J]. Acta Geologica Sinica, 2012,86(9):1447-1478.
[31] ������,������,������,��.��������ͨǰ�����BIF�����о�:��չ������[J].��ʯѧ��,2012,28(11):3431-3445. ZHANG Lian-chang,ZHAI Ming-guo,WAN Yu-sheng,et al.Study of the Precambrian BIF-iron deposits in the North China Craton:progresses and questions[J]. Acta Petrologica Sinica, 2012,28(11):3431-3445.
[32] ������,��Ρ,������,��.��������ͨ��������̫�Ŵ����ڵؿ�����:���԰�ʯ����������ѧ��Hfͬλ�ص�֤��[J].��ʯѧ��,2016,32(9):2839-2855. LI Peng-chuan,GUO Wei,LIU Zheng-hong,et al.Late Neoarchean crustal growth in the northeast of the North China Craton:evidence from the geochronology and Hf isotope composition of Banshigou supracrustal rocks[J]. Acta Petrologica Sinica,2016,32(9):2839-2855.
[33] �˹���,Ф���,½����,��.�й���ع��쵥Ԫ����[J].�й�����,2009,36(1):1-28. PAN Gui-tang,XIAO Qing-hui,LU Song-nian,et al.Subdivision of tectonic units in China[J].Geology in China, 2009,36(1):1-28.
[34] ��ɾ�,���Ӻ�,������.LA-MC-ICP-MS�ʯ΢��ԭλU-Pb���꼼��[J]. �󴲵���, 2009.28(4):481-492. HOU Ke-jun,LI Yan-he,TIAN You-rong.In situ U-Pb zircon dating using Laser Ablation-Multi ion Counting-ICP-MS[J]. Mineral Deposits,2009,28(4):481-492.
[35] ��ɾ�,���Ӻ�,������,��.LA-MC-ICP-MS�ʯHfͬλ�صķ������������Ӧ��[J].��ʯѧ��, 2007,23(10):2595-2604. HOU Ke-jun,LI Yan-he,ZOU Tian-ren,et al.Laser ablation LA-MC-ICP-MS technique for Hf isotope microanalysis of zircon and its geological applications[J]. Acta Petrologica Sinica, 2007,23(10):2595-2604.
[36] Morel M L A, Nebel O, Nebel-Jacobsen Y J,et al.Hafnium isotope characterization of the GJ-1 zircon reference material by solution and laser-ablation MC-ICPMS[J].Chemical Geology, 2008,255(1):231-235.
[37] Liu Y S, Hu Z C, Zong K Q,et al.Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS[J]. Chinese Science Bulletin, 2010,55(15):1535-1546.
[38] Ludwing K R.Users manual for Isoplot/EX (Rev.2.49):a geochronological toolkit for Microsoft Excel[J].Berkeley:berkeley Geochronology Center Special Publication, 2001:1-55.
[39] Wang C Y,Campbell I H,Allen C M,et al.Rate of growth of the preserved North American continental crust:evidence from Hf and O isotopes in Mississippi detrital zircons[J].Geochimica et Cosmochimica Acta,2009,73(3):712-728.
[40] Söderlund U, Patchett P J, Vervoort J D,et al.The 176Lu decay constant determined by Lu-Hf and U-Pb isotope systematics of Precambrian mafic intrusions[J]. Earth and Planetary Science Letters,2004,219(3/4):311-324.
[41] Blichert-Toft J,Albarède F.The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle-crust system[J]. Earth and Planetary Science Letters, 1997,148(1/2):243-258.
[42] Griffin W L, Pearson, N J, Belousova E,et al.The Hf isotope composition of cratonic mantle:LA-MC-ICP-MS analysis of zircon megacrysts in kimberlites[J].Geochimica et Cosmochimica Acta, 2000,64(1):133-147.
[43] Barker F,Arth J G.Generation of trondhjemitic-tonalitic liquidsand Archean bimodal trondhjemite-basalt suites[J].Geology,1976,10(4):596-600.
[44] Peccerillo A,Taylor S R.Geochemistry of Eocene calc-alkaline volcanic rocks from Kastamonu area,Northern Turkey[J].Contributions to Mineralogy and Petrology,1976,58(1):63-81.
[45] Middlemost E A K. Magmas and magmatic rocks:an introduction to igneous petrology[M]. Longman, 1985:1-85.
[46] Wedepohl K H.The composotion of the continental crust[J].Geochimica et Cosmochimica Acta,1995,59:1217-1232.
[47] Boynton W V.Cosmochemistry of the rare earth elements:meteorite studies[J].Developments in Geochemistry, 1984,2(2):63-114.
[48] Sun S S,Mcdonough W F.Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and processes[J]. Geological Society,1989,42(1):313-345.
[49] Defant M J,Drummond M S.Derivation of some morden arc magmas by of young subducted lithosphere[J].Nature,1990,347:662-665.
[50] Tarney J.Geochemistry of Archaean high grade gneisses,with implications as to origin and evolution of the Precambrian crust[C]//Windley B F.The early history of Earth.London:John Wiley & Sons,1976:1.
[51] ������,���п�,֣����,��.���ɹ��в�С�Ϲ�-���ǹ�������̫�Ŵ�TTG��ϵ�����������[J].��ʯѧ��,2006,22(11):2762-2768. ZHANG Yong-qing,ZHANG You-kuan,ZHENG Bao-jun,et al.Geological character and significance of Adakite and TTG in Xiaonangou-Mingxinggou district in central of Inner Mongolia[J].Acta Petrologica Sinica,2006,22(11)2762-2768.
[52] ��ΰ,������,������,��.����ɽ�ˮ������TTGϵ����ʯ���ʯSHRIMP���ѧ�͵���ѧ�����������[J].��Ȼ��ѧ��չ,2005,15(12):1476-1484. TIAN Wei,LIU Shu-wen,LIU Chao-hui,et al.Zircon SHRIMP geochronology and geochemistry of TTG rocks in Sushui Complex from Zhongtiao Mountain with its geological implications[J].Progress in Nature Science,2005,15(12):1476-1484.
[53] ������,����һ,������,��.�Ƿ������ǰ����͵ؿ��ݻ�:����ѧ���ʯSHRIMP U-Pb���ѧ��Լ[J].����ѧ��,2009b,83(7):982-999. WAN Yu-sheng,LIU Dun-yi,WANG Shi-yan,et al.Early Precambrian crustal evolution in the Dengfeng area,Henan Province(eastern China):constraints from geochemistry and SHRIMP U-Pb zircon dating[J].Acta Geologica Sinica, 2009b,83(7):982-999.
[54] ����¡,˾�پ�,ë����,��.��ɽ��ׯ������̫�Ŵ�TTG��ʯ�������������[J].�ƽ��ѧ����,2016,24(2):51-58. LI Xing-long,SI Rong-jun,MAO Guang-yu,et al.Neoarchaean TTG petrogenesis in Mazhuang,Songshan area and its geological significance[J].Gold Science and Technology,2016,24(2):51-58.
[55] ���Ͻ�,������,����.��������ͨ��Ե���������̫�Ŵ�TTG�������:��������Ҳ�ͬ��������ڵIJ���[J].����ͨ��,2012,31(5):686-695. LI Meng-jiang,WANG Ren-min,ZHANG Li.The genesis of Neoarchean TTG in the Shangyi area of the northern margin of North China Craton:melt from basalt of oceanic crust at varying depth[J]. Geological Bulletin of China, 2012, 31(5):686-695.
[56] Nutman A P,Wan Y S,Du L L,et al.Multistage Late Neoarchaean crustal evolution of the North China Craton,eastern Hebei[J].Precambrian Research,2011,189(1):43-65.
[57] ������,������,��ΰ,��.³������ʯ��ɽ-����ɽ������ʯSHRIMP U-Pb���꼰�γ�ʱ��[J].ɽ��������Դ,2010,26(9):1-11. WANG Shi-jin,WAN Yu-sheng,WANG Wei,et al.Zircon SHRIMP U-Pb dating and the forming age of Shimenshan-Fengxianshan rock in western Shandong[J].Shandong Land and Resources,2010,26(9):1-11.
[58] ������,������,����,��.������̫�Ŵ�����Ƭ���ҵ���ʯ����ѧ�����ͳ���ָʾ[J].��ʯѧ��,2013,29(7):2295-2312. SHAN Hou-xiang,ZHAI Ming-guo,WANG Fang,et al.Geochemical characteristics and petrogenesis of the two types of Neoarchean gneisses from the Jiaobei terrane[J]. Acta Petrologica Sinica,2013,29(7):2295-2312.
[59] Rapp R P,Shimizu N,Norman M D,et al.Reaction between slab-derived melts and peridotite in the mantle wedge:experimental constraints at 3.8 Gpa[J]. Chemical Geology,1999,160(4):335-356.
[60] Smithies R H.The Archean tonalite-trondhjemite-granodiorite(TTG) series is not an analogue of Cenozoic adakite[J]. Earth and Planetary Science Letters,2000,182(1):115-125.
[61] Ǯ����.��ǰ����ʹ�½�ؿǵ������빹���ݻ�����[J].��ʯѧ��,1996,12(2):169-178. QIAN Xiang-lin.The nature of the Early Precambrian continental crust and its tectonic evolution model[J].Acta Petrologica Sinica, 1996,12(2):169-178.
[62] Ǯ����,���,���ػ�.ǰ����ʹ�½�ؿǵ��ʹ����ݻ��о���չ������[J].��У����ѧ��,2005,11(2):145-153. QIAN Xiang-lin,LI Jiang-hai,CHENG Su-hua.A review on Precambrian tectonic evolution of continental crust[J].Geological Journal of China Universities,2005,11(2):145-153.
[63] Arndt N T,Goldstein S L.An open boundary between lower continental crust and mantle:its role in crust formation and crustal recycling[J].Tectonophysics,1989,161(3/4):201-212.
[64] Kröner A,Layer P W.Crust formation and plate motion in the Early Archean[J]. Science,1992,256(5062):1405-1411.
[65] Martin H.Petrogenesis of Archaean trondhjemites,tonalites,and granodiorites from eastern Finland:major and trace element geochemistry[J].Journal of Petrology,1987,28(5):921-953.
[66] Jiang N,Liu Y S,Zhou W G,et al.Derivation of Mesozoic adakitic magmas from ancient lower crust in the North China Craton[J].Geochimica et Cosmochimica Acta,2007,71(10):2591-2608.
[67] Moyen J F.The composite Archaean grey gneisses:petrological significance, and evidence for a non-unique tectonic setting for Archaean crustal growth[J]. Lithos, 2011,123(1/4):21-36.
[68] Rapp R P,Watson E B.Dehydration melting of metabasalt at 8~32 kbar:implications for continental growth and crust-mantle recycling[J].Journal of Petrology,1995,36(4):891-931.
[69] ������,�α�,��Ԫ��,��.�ɱ���˳-��ԭ����̫������׵���ѧ������������������[J].��������,2005,51(2):128-137. WAN Yu-sheng,SONG Biao,GENG Yuan-sheng,et al.Geochemical characteristics of Archaean basement in the Fushun-Qingyuan Area, northern Liaoning Province and its geological significance[J],Geological Review,2005,51(2):128-137.
[70] ������,�α�,��Ԫ��,��.�ɱ���˳-��ԭ����̫������ʯSHRIMP�ʯU-Pb���ѧ�����������[J].����ѧ��,2005,79(1):78-87. WAN Yu-sheng,SONG Biao,GENG Yuan-sheng,et al.Zircon SHRIMP U-Pb geochronology of Archaean rocks from the Fushun-Qingyuan area, Liaoning Province and its geological significance[J].Acta Geologica Sinica,2005,79(1):78-87.
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