Journal of Jilin University(Earth Science Edition) ›› 2017, Vol. 47 ›› Issue (1): 126-138.doi: 10.13278/j.cnki.jjuese.201701112

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Discovery of the Late Cambrian Intermediate-Basic Volcanic Rocks in Tahe, Northern Da Hinggan Mountain and Its Geological Significance

Wang Yan, Yang Xiaoping, Na Fuchao, Fu Junyu, Sun Wei, Yang Fan, Liu Yingcai, Zhang Guangyu, Song Weimin, Yang Yajun, Qian Cheng, Pang Xuejiao   

  1. Shenyang Institute of Geology and Mineral Resources, CGS, Shenyang 110034, China
  • Received:2016-05-25 Online:2017-01-26 Published:2017-01-26
  • Supported by:
    Supported byGeological Survey Project of China Geological Survey(DD20160201-01,1212011220435,DD20160343-08,DD20160343-09,1212011085210,DD20160345-17)

Abstract: There exist a set of intermediate-basic volcanic rocks in Tahe, north east part of Erguna massif,which consist of basaltic-andestite, basaltic-trachyandesite and trachybasalt. This set of volcanic rocks was previously allocated to the Middle-Late Jurassic Tamulangou Formation. However, according to the 206Pb/238U isotope of zircon determination data of (501.1±1.4) Ma (n=23) and (500.50±0.95) Ma(n=14)for basaltic-andestite and trachybasalt, it is the first reported existence of Cambrian volcanic rocks north of Tahe. Intermediate-basic volcanic shows the sub alkalne shoshonite series feature, and without any metamorphose; negative Eu anomalies, (La/Yb)N=16.63-25.91; Rich Ba, Rb, Sr, and K and depletion Nb,Ta,Ti. The magma is likely related to the extension in the island-arc background, and it is considered that there exists the Cambrian in the certain range of this area. The research results provide new materials for re-evaluating the Mesozoic volcanic rocks in local area of northern Da Hing gan, discussing the evolution history of Xinlin-Xiguitu fault, and the continental crust evolution of Erguna massif at the southwest edge of the Siberia plate.

Key words: Da Hinggan Mountain, Tahe area, Late Cambrian, basalt-andesite, zircons U-Pb geochronology

CLC Number: 

  • P588.14
[1] 张吉衡.大兴安岭地区中生代火山岩的年代学格架[D].长春:吉林大学,2006. Zhang Jiheng. Geochronological Framework of the Mesozoic Volcano Rock in Dahinggan Mts[D]. Changchun:Jilin University, 2006.
[2] 赵忠华,孙德有,苟军,等.满洲里南部塔木兰沟组火山岩年代学与地球化学[J].吉林大学学报(地球科学版),2011,41(6):1865-1880. Zhao Zhonghua, Sun Deyou, Gou Jun, et al. Chronology and Geochemistry of Volcanic Rocks in Tamulangou Formation from Southern Manchuria, Inner-Mongolia[J]. Journal of Jilin University (Earth Science Edition), 2011, 41(6):1865-1880.
[3] 孟恩,许文良,杨德彬,等.满洲里地区灵泉盆地中生代火山岩的锆石U-Pb年代学地球化学及其地质意义[J].岩石学报,2011,27(4):1209-1226. Meng En, Xu Wenliang, Yang Debin, et al. Zircon U-Pb Chronology, Geochemistry of Mesozoic Volcanic Rocks from the Lingquan Basin in Manzhouli Area, and Its Tectonic Implications[J]. Acta Petrologica Scinica, 2011, 27(4):1209-1226.
[4] Zhou J B,Wilde S A. The Crustal Accretion History and Tectonic Evolution of the NE China Segment of the Central Asian Orogenic Belt[J]. Gondwana Research, 2013, 23(4):1365-1377.
[5] 周建波,石爱国,景妍.东北地块群构造演化与古大陆重建[J].吉林大学学报(地球科学版),2016,46(4):1042-1055. Zhou Jianbo,Shi Aiguo,Jing Yan. Combined NE China Blocks:Tectonic Evolution and Supercontinent Reconstructions[J]. Journal of Jilin University (Earth Science Edition), 2016, 46(4):1042-1055.
[6] 张兆忠,冯锦江,张秉良,等.中国的蓝片岩和板块构造[J].岩石学报,1986,2(4):31-40. Zhang Zhaozhong, Feng Jinjiang, Zhang Bingliang, et al. Glaucophane Schist in China and Plate Tectonics[J]. Acta Petrologica Sinica, 1986, 2(4):31-40.
[7] 徐备,赵盼,鲍庆中,等.兴蒙造山带前中生代构造单元划分初探[J]. 岩石学报,2014,30(7):1841-1857. Xu Bei, Zhao Pan, Bao Qingzhong, et al. Preliminary Study on the Pre-Esozoic Tectonic Unit Division of the Xing-Meng Orogenic Belt (XMOB)[J]. Acta Petrologica Sinica, 2014, 30(7):1841-1857.
[8] 李瑞山.新林蛇绿岩[J].黑龙江地质,1991, 2(1):19-31. Li Ruishan. Xinlin Ophiolite[J]. Heilongjiang Geology, 1991, 2(1):19-32.
[9] 张丽,刘永江,李伟民,等.关于额尔古纳地块基底性质和东界的讨论[J].地质科学,2013,28(1):227-244. Zhang Li, Liu Yongjiang, Li Weimin, et al. Discussion on the Basement Properties and East Boundary of the Ergun Massif[J]. Chinese Journal of Geology, 2013, 28(1):227-244.
[10] 葛文春,吴福元,周长勇,等.大兴安岭北部塔河花岗岩体的时代及对额尔古纳地块构造归属的制约[J].科学通报,2005,50(12):1239-1247. Ge Wenchun, Wu Fuyuan, Zhou Changyong, et al. Emplacement Age of the Tahe Granite and Its Constraints of the Da Hinggan Mountains[J]. Chinese Science Bulletin, 2005, 50(12):1239-1247.
[11] 武广,孙丰月,赵财胜,等.额尔古纳地块北缘早古生代后碰撞花岗岩的发现及其地质意义[J]. 科学通报,2005,50(20):2278-2288. Wu Guang, Sun Fengyue, Zhao Caisheng, et al. The Granite of Post-Collision and Its Geological Significance of Early Paleozoic Northern Margin in Eerguna Block[J]. Chinese Science Bulletin, 2005, 50(20):2278-2288.
[12] Wilson B M. Igneous Petrogenesis[M]. London:Un-win Hyman, 1989:1-25.
[13] Irvine I N. A Guide to the Chemical Classification of the Common Volcanic Rocks, Can[J].J Earth Sci, 1971, 8:532-548.
[14] Pearce J A. Statistical Analysis of Major Element Patterns in Basalts[J].J Petro, 1976, 17:15-43.
[15] Le Bas M J, Le Maitre R W, Streckeisen A, et al. A Chemical Classification of Volcanic Rocks Based on the Total Alkali-Silica Diagram[J]. Journal of Petrology, 1986, 27(3):745-750.
[16] Pearceillo A, Taylor R. Geochemistry of Eocene Cale-Alkaline Volcanic Rocks from the Kastamenu Area Northeron Tukey[J]. Contrib, Mineral, Petrol, 1976, 58(1):63-81.
[17] Boynton W V. Geochemistry of the Rare Earth Ele-ments:Meteorite Studies[C]//Henderson P. Rare Earth Element Geochemistry. Amsterdam:Elservier,1984:63-114.
[18] 李曙光.大陆俯冲化学地球动力学[C]//郑永飞.化学地球动力学.北京:科学出版社,1999:334-357. Li Shuguang. Continental Subduction and Chemical Kinetics[C]//Zheng Yongfei. Chemical Geodynamics. Beijing:Science Press, 1999:334-357.
[19] Sun, McDonough. Chemical and Isotopic Systematics of Ocean Basalts Implications for Mantle Composition and Processes[C]//Saunders A D,Norry M J.Magmatism in Ocean Basms Geo Soc. London:Spec Publ, 1989(42):313-345.
[20] Rudnick R L, Fountain D M. Nature and Compo-sition of the Continental Crust:A Lower Crustal Perspective[J]. Reviews of Geophysics, 1995, 33(3):267-309.
[21] 李毅,吴泰然,罗红玲,等.内蒙古四子王旗早白垩世钾玄岩的地球化学特征及其形成构造环境[J].岩石学报,2006,22(11):2791-2800. Li Yi, Wu Tairan, Luo Hongling, et al. Geochemistry and Tectonic Setting of the Early Cretaceous Shoshonite of Siziwangqi Area, Inner Mongolia[J]. Acta Petrologica Scinica, 2006, 22(11):2791-2800.
[22] Stolz A I, Jochum K P, Spettel B, et al.Fluid-and Melt-Related Enrichment in the Subare Mantle Evidence from Nb/Ta Variations in Island-Arc Basalts[J]. Geology, 1996, 24(7):587-590.
[23] Pearce T H,Gorman B E,Birkett T C,et al. The Relationship Between Major Element Chemistry and Tectonic Environment of Basic and Intermediate Volcanic Rocks[J]. Earth and Planetary Science Letters, 1977, 36:121-132.
[24] Wood D A. The Application of a Th-Hf-Ta Diagram to Problems of Tectonomagmatic Classfication and to Establishing the Nature of Crystal Contamination Basaltic Lavas of the British Tertiaty Volcanic Province[J]. Earth and Planetary Science Letters,1980, 50(5/6):11-30.
[25] Liu Y S, Gao S, Hu Z C,et al. Continental and Oceanic Crust Recyling-Incluced Melt-Peridotite Interactions in the Trans-North China Orogen:U-Pb Dating, Hf Isotopes and Trace Elements in Zircon from Mantle Xenoliths[J]. Journal of Petrology, 2010, 51(1/2):537-571.
[26] Ludwig K R. A Geochronological Toolkit for Mic-rosoft Excel[R]. Berkeley:Berkeley Geochronology Center, 2003:1-56.
[27] 李怀坤,耿建珍,郝爽,等.用激光烧蚀多接收器等离子体质谱仪(LA-MC-ICPMS)测定锆石U-Pb同位素年龄的研究[J].矿物学报,2009,29(增刊1):600-601. Li Huaikun, Geng Jianzhen, Hao Shuang, et al. Study on Determination of Zircon U-Pb Isotopic Age of Laser Ablation Multicollector Inductively Coupled Plasma Mass Spectrometry[J]. Journal of Minerals, 2009, 29(Sup.1):600-601.
[28] 王东方.中国东部中亚构造带及向环太平洋构造带的转化[J].华北地质矿产杂志, 1995,10(2):135-142.Wang Dongfang. A Diseussion on the Tectonic Zone of Middle Asia and Its Transformation to Tectonic Zone of Circim Paeific Ocean in Eastern China[J]. Issue of Geology and Resource of North China, 1995, 10(2):135-142.
[29] 王鸿祯,何国琦,张世红.中国与蒙古之地质[J].地学前缘,2006,13(6):1-13. Wang Hongzhen, He Guoqi, Zhang Shihong. The Geology of China and Mongolia[J]. Earth Science Frontiers, 2006, 13(6):1-13.
[30] Wu G,Chen Y C,Chen Y J, et al. Zircon U-Pb Ages of the Metamorphic Supracrustal Rocks of the Xinghuadukou Group Andgranitic Complexes in the Argun Massif of the Northern Great Hinggan Range,NE China,and Their Tectonic Implications[J]. Journal of AsianEarth Sciences, 2012(49):214-233.
[31] Wu F Y, Sun D Y, Ge W C, et al. Geochronology of the Phanerozoic Granitoids Innortheastern China[J]. Journal of Asian Earth Sciences, 2011(41):1-30.
[32] Zhou J B, Wilde S A, Zhang X Z, et al. Early Pal-eozoic Metamorphic Rocks of the Erguna Block in the Great Xing'an Range,NE China:Evidence for the Timing of Magmatic and Metamorphic Events and Their Tectonic Implications[J]. Tectonophysics,2011, 499:105-117.
[33] 黑龙江省地质矿产局.黑龙江省区域地质志[M].北京:地质出版社,1993. Heilongjiang Bureau of Geology and Mineral Resources. Regional Geology of Heilongjiang Province[M]. Beijing:Geological Publishing House, 1993.
[34] 苗来成,范蔚茗,张福勤,等.小兴安岭西北部新开岭-科洛杂岩锆石SHRIMP年代学研究及其意义[J].科学通报,2003,48(22):2315-2323. Miao Laicheng, Fan Weiming, Zhang Fuqin, et al. Xinkailing-Kolo Complex Zircon SHRIMP Geochronology Research and Its Significance in Northwest Xiaoxin'anling[J]. Science Bulletin of China, 2003, 48(22):2315-2323.
[35] 叶惠文,张兴洲,周裕文.从蓝片岩及蛇绿岩特点看满洲里-绥芬河断面岩石圈结构与演化[C]//M-SGT地质课题组.中国满洲里-绥芬河地学断面域内岩石圈结构及其演化的地质研究.北京:地震出版社, 1994:73-83. Ye Huiwen, Zhang Xingzhou, Zhou Yuwen. Study on the LithosphereStructure and Evolution of Manchuria-Suifenhe Section from the Perspective of Blue Schist and Ophiolite Characteristics[C]//M-SGT the Geological Task Group. Study on the Structure and Evolution of the Lithosphere in the Area of Manchuria Suifenhe, China. Beijing:Seismological Press, 1994:73-83.
[36] 秦秀峰,尹志刚,汪岩,等.大兴安岭北端漠河地区早古生代埃达克质岩特征及地质意义[J].岩石学报,2007,23(6):1501-1511. Qin Xiufeng, Yin Zhigang, Wang Yan, et al.Early Paleozoic Adakitic Rocks in Mohe Area at the Northern End of the DaHinggan Mountains and Their Geological Significance[J]. Acta Petrologica Sinica, 2007, 23(6):1501-1511.
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