Institute of Geomechanics, Chinese Academy of Geological SciencesHost
Advanced Search
Previous Article Next Article
2017 Vol. 23, No. 3
Article Contents
Article navigation > Journal of Geomechanics > 2017 > 23(3): 382-396
Next Article Previous Article

WANG Wen-long, TENG Xue-jian, LIU Yang, TENG Fei, GUO Shuo, HE Peng, TIAN Jian, DUAN Xiao-long. ZIRCON U-PB CHRONOLOGY AND GEOCHEMICAL CHARACTERISTICS OF THE WUHEERTU GRANITE MASS IN LANGSHAN, INNER MONGOLIA[J]. Journal of Geomechanics, 2017, 23(3): 382-396.
Citation: WANG Wen-long, TENG Xue-jian, LIU Yang, TENG Fei, GUO Shuo, HE Peng, TIAN Jian, DUAN Xiao-long. ZIRCON U-PB CHRONOLOGY AND GEOCHEMICAL CHARACTERISTICS OF THE WUHEERTU GRANITE MASS IN LANGSHAN, INNER MONGOLIA[J]. Journal of Geomechanics, 2017, 23(3): 382-396.
shu

ZIRCON U-PB CHRONOLOGY AND GEOCHEMICAL CHARACTERISTICS OF THE WUHEERTU GRANITE MASS IN LANGSHAN, INNER MONGOLIA

  • Tianjin Center of Geological Survey, CGS, Tianjin 300170, China

Received Date:  24 September 2016
Publish Date:  25 June 2017
    Abstract

  • The WuheErtu granite mass, with the main rock types of syenogranite and monzogranite, are distributed in Langshan area, Inner Mongolia, northern margin of the North China Plate. Zircon U-Pb ageis 236.1±1.0Ma, indicating the WuherErtu granite mass formed in late Triassic.Geochemical results show high content of SiO2(71.94~73.91%), K2O+Na2O(8.34~8.88%), low content of Ca and Mg, and weak content of aluminum(0.98 < A/CNK < 1.07). In SiO2-K2O diagram, sample points fall into the transitional region between high-K calc-alkaline and Shoshonite series. In the primitive mantle-normalized spider diagram, the geochemical characteristics of the granite mass show in some degree enrichment in Rb、Th、K、Nd、Zr、Hf、Sm and depletion in Ba、Nb、Ta、Sr、P、Ti, with medium to negligible Eu anomalies (δEu=0.47~0.66), which indicate the WuherErtu granite mass belong to the post-collisional granite formed in the tectonic setting transformed from compression system to extension system. Zircon Hf isotopic displays that εHf(t) values vary from -20.6 to +7.6 and Hf model ages (TDM2) vary from 780~2559 Ma, which suggest a mixed magma source of old continental crust with a small involvement of juvenile components.The comprehensive study of this granite mass helps to further understand and explore the tectonic-magmatic evolution of the northern margin of the North China plate in late Permian-Triassic.

    • FullText(HTML)
  • 加载中
    • References
  • [1] Cawood P A, Kröner A, Collins W J, et al. Accretionary orogens through Earth history[A]. Cawood P A, Kröner A. Earth Accretionary Systems in Space and Time[M].Geological Society, London, Special Publications, 2009, 318(1):1~36.

    Google Scholar

    [2] Xiao W J, Windley B F, Yuan C, et al. Paleozoic multiple subduction-accretion processes of the southern Altaids[J]. American Journal of Science, 2009, 309(3):221~270. doi: 10.2475/03.2009.02

    CrossRef Google Scholar

    [3] Windley B F, Alexeiev D, Xiao W J, et al. Tectonic models for accretion of the Central Asian Orogenic Belt[J]. Journal of the Geological Society, 2007, 164(1):31~47. doi: 10.1144/0016-76492006-022

    CrossRef Google Scholar

    [4] Kovalenko V I, Yarmolyuk V V, Kovach V P, et al. Isotope provinces, mechanisms of generation and sources of the continental crust in the Central Asian mobile belt:Geological and isotopic evidence[J]. Journal of Asian Earth Sciences, 2004, 23(5):605~627. doi: 10.1016/S1367-9120(03)00130-5

    CrossRef Google Scholar

    [5] Jahn B M, Wu F Y, Chen B. Massive granitoid generation in Central Asia:Nd isotope evidence and implication for continental growth in the Phanerozoic[J]. Episodes, 2000, 23(2):82~92.

    Google Scholar

    [6] Xu B, Charvet J, Chen Y, et al. Middle Paleozoic convergent orogenic belts in western Inner Mongolia (China):Framework, kinematics, geochronology and implications for tectonic evolution of the Central Asian Orogenic Belt[J]. Gondwana Research, 2013, 23(4):1342~1364. doi: 10.1016/j.gr.2012.05.015

    CrossRef Google Scholar

    [7] Zhang X, Gao Y, Wang Z, et al. Carboniferous appinitic intrusions from the northern North China craton:Geochemistry, petrogenesis and tectonic implications[J]. Journal of the Geological Society, 2012, 169(3):337~351. doi: 10.1144/0016-76492011-062

    CrossRef Google Scholar

    [8] Xu Z, Han B F, Ren R, et al. Ultramafic-mafic mélange, island arc and post-collisional intrusions in the Mayile Mountain, West Junggar, China:Implications for Paleozoic intra-oceanic subduction-accretion process[J]. Lithos, 2012, 132~133:141~161. doi: 10.1016/j.lithos.2011.11.016

    CrossRef Google Scholar

    [9] Han B F, He G Q, Wang X C, et al. Late Carboniferous collision between the Tarim and Kazakhstan-Yili Terranes in the western segment of the South Tian Shan Orogen, Central Asia, and implications for the Northern Xinjiang, western China[J]. Earth-Science Reviews, 2011, 109(3/4):74~93.

    Google Scholar

    [10] Fu D, Huang B, Peng S B, et al. Geochronology and geochemistry of Late Carboniferous volcanic rocks from northern Inner Mongolia, North China:Petrogenesis and tectonic implications[J]. Gondwana Research, 2016, 36:545~560. doi: 10.1016/j.gr.2015.08.007

    CrossRef Google Scholar

    [11] Zhang W, Wu T R, Zheng R G, et al. Post-collisional Southeastern Beishan granites:Geochemistry, geochronology, Sr-Nd-Hf isotopes and their implications for tectonic evolution[J]. Journal of Asian Earth Sciences, 2012, 58:51~63. doi: 10.1016/j.jseaes.2012.07.004

    CrossRef Google Scholar

    [12] Luo H L, Wu T R, Zhao L, et al. Permian high Ba-Sr granitoids:Geochemistry, age and tectonic implications of Erlangshan Pluton, Urad Zhongqi, Inner Mongolia[J]. Acta Geologica Sinica (English Edition), 2009, 83(3):603~614. doi: 10.1111/j.1755-6724.2009.00054.x

    CrossRef Google Scholar

    [13] 罗红玲, 吴泰然, 赵磊.华北板块北缘乌梁斯太A型花岗岩体锆石SHRIMP U-Pb定年及构造意义[J].岩石学报, 2009, 25(3):515~526.

    Google Scholar

    LUO Hong-ling, WU Tai-ran, ZHAO Lei. Zicron SHRIMP U-Pb dating of Wuliangsitai A-type granite on the northern margin of the North China Plate and tectonic significance[J]. Acta Petrologica Sinica, 2009, 25(3):515~526.

    Google Scholar

    [14] Tang K D. Tectonic development of Paleozoic foldbelts at the north margin of the Sino-Korean Craton[J]. Tectonics, 1990, 9(2):249~260. doi: 10.1029/TC009i002p00249

    CrossRef Google Scholar

    [15] Zhang S H, Zhao Y, Liu J M, et al. Different sources involved in generation of continental arc volcanism:The Carboniferous-Permian volcanic rocks in the northern margin of the North China block[J]. Lithos, 2016, 240~243:382~401. doi: 10.1016/j.lithos.2015.11.027

    CrossRef Google Scholar

    [16] Wilde S A. Final amalgamation of the Central Asian Orogenic Belt in NE China:Paleo-Asian Ocean closure versus Paleo-Pacific plate subduction-A review of the evidence[J]. Tectonophysics, 2015, 662:345~362. doi: 10.1016/j.tecto.2015.05.006

    CrossRef Google Scholar

    [17] Wang Z J, Xu W L, Pei F P, et al. Geochronology and geochemistry of middle Permian-Middle Triassic intrusive rocks from central-eastern Jilin Province, NE China:Constraints on the tectonic evolution of the eastern segment of the Paleo-Asian Ocean[J]. Lithos, 2015, 238:13~25. doi: 10.1016/j.lithos.2015.09.019

    CrossRef Google Scholar

    [18] Jian P, Liu D Y, Kröner A, et al. Evolution of a Permian intraoceanic arc-trench system in the Solonker suture zone, Central Asian Orogenic Belt, China and Mongolia[J]. Lithos, 2010, 118(1/2):169~190.

    Google Scholar

    [19] Zhang S H, Zhao Y, Song B, et al. Contrasting Late Carboniferous and Late Permian-Middle Triassic intrusive suites from the northern margin of the North China craton:Geochronology, petrogenesis, and tectonic implications[J]. GSA Bulletin, 2009, 121(1/2):181~200.

    Google Scholar

    [20] Zhang S H, Zhao Y, Kröner A, et al. Early Permian plutons from the northern North China Block:constraints on continental arc evolution and convergent margin magmatism related to the Central Asian Orogenic Belt[J]. International Journal of Earth Sciences, 2009, 98(6):1441~1467. doi: 10.1007/s00531-008-0368-2

    CrossRef Google Scholar

    [21] Chen B, Jahn B M, Tian W. 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[J]. Journal of Asian Earth Sciences, 2009, 34(3):245~257. doi: 10.1016/j.jseaes.2008.05.007

    CrossRef Google Scholar

    [22] Jian P, Liu D Y, Kröner A, et al. Time scale of an early to mid-Paleozoic orogenic cycle of the long-lived Central Asian Orogenic Belt, Inner Mongolia of China:Implications for continental growth[J]. Lithos, 2008, 101(3/4):233~259.

    Google Scholar

    [23] Xiao W J, Windley B F, Hao J, et al. Accretion leading to collision and the Permian Solonker suture, Inner Mongolia, China:Termination of the central Asian orogenic belt[J]. Tectonics, 2003, 22(6):123~136.

    Google Scholar

    [24] Chen B, Jahn B M, Wilde S, et al. Two contrasting paleozoic magmatic belts in northern Inner Mongolia, China:petrogenesis and tectonic implications[J]. Tectonophysics, 2000, 328(1/2):1069.

    Google Scholar

    [25] Liégeois J P. Preface-some words on the post-collisional magmatism[J]. Lithos, 1998, 45:15~18.

    Google Scholar

    [26] Liu M, Zhang D, Xiong G Q, et al. Zircon U-Pb age, Hf isotope and geochemistry of Carboniferous intrusions from the Langshan area, Inner Mongolia:Petrogenesis and tectonic implications[J]. Journal of Asian Earth Sciences, 2016, 120:139~158. doi: 10.1016/j.jseaes.2016.01.005

    CrossRef Google Scholar

    [27] Wang Z Z, Han B F, Feng L X, et al. Geochronology, geochemistry and origins of the Paleozoic-Triassic plutons in the Langshan area, western Inner Mongolia, China[J]. Journal of Asian Earth Sciences, 2015, 97:337~351. doi: 10.1016/j.jseaes.2014.08.005

    CrossRef Google Scholar

    [28] Lin L N, Xiao W J, Wan B, et al. Geochronologicand Geochemicalevidenceforpersistence of South-dipping subduction to Late Permian time, Langshan area, Inner Mongolia(China):Significance for termination of accretionary orogenesis in the Southern Altaids[J]. American Journal of Science, 2014, 314(2):679-703. doi: 10.2475/02.2014.08

    CrossRef Google Scholar

    [29] 吴亚飞, 曾键年, 曹建劲, 等.内蒙古东升庙海西期岩体锆石U-Pb年龄及Hf同位素特征[J].地质科技情报, 2013, 32(6):22~29.

    Google Scholar

    WU Ya-fei, ZENG Jian-nian, CAO Jian-jin, et al. Zircon U-Pb ages and Hf isotopes of hercynian intrusion in Dongshengmiao, Inner Mongolia[J]. Geological Science and Technology Information, 2013, 32(6):22~29.

    Google Scholar

    [30] 刘晔, 钱建强, 杨斌.内蒙古东升庙一带花岗质岩体锆石年代学及其构造意义[J].甘肃地质, 2013, 22(4):37~44.

    Google Scholar

    LIU Ye, QIAN Jian-qiang, YANG Bin. Zircon geochronology of granitic mass in Dongshengmiao of Inner Mongolia and tectonic significance[J]. Gansu Geology, 2013, 22(4):37~44.

    Google Scholar

    [31] 于延秋, 郭守钰, 王立峰.内蒙古狼山浩日格山海西期花岗岩体特征与形成环境[J].世界地质, 2011, 30(3):345~351.

    Google Scholar

    YU Yan-qiu, GUO Shou-yu, WANG Li-feng, et al. Characteristics and formation environment of Hercynian granites in Haorigeshan of Langshan, Inner Mongolia[J]. Global Geology, 2011, 30(3):345~351.

    Google Scholar

    [32] 鲁有朋, 俞胜, 张永全, 等.内蒙狼山地区中生代构造演化及年代学特征[J].甘肃地质, 2015, 24(2):24~29.

    Google Scholar

    LU You-peng, YU Sheng, ZHANG Yong-quan, et al. Tectonic evolution and chronology constrains of Langshan region in Inner Mongolia autonomous[J]. Gansu Geology, 2015, 24(2):24~29.

    Google Scholar

    [33] 高洪雷. 内蒙古狼山地区中生代构造演化与年代学约束[D]北京: 中国地质大学(北京), 2010.http://cdmd.cnki.com.cn/Article/CDMD-11415-2010085195.htm

    Google Scholar

    GAO Hong-lei. Structure evolution and chronology constrains of Lang Shan in Neimeng autonomous region[D]. Beijing:China University of Geosciences (Beijing), 2010.

    Google Scholar

    [34] Sengör A M C, Natal' In B A, Burtman V S. Evolution of the Altaid tectonic collage and Palaeozoic crustal growth in Eurasia[J]. Nature, 1993, 364(6435):299~307. doi: 10.1038/364299a0

    CrossRef Google Scholar

    [35] Shi X J, Wang T, Zhang L, et al. Timing, petrogenesis and tectonic setting of the Late Paleozoic gabbro-granodiorite-granite intrusions in the Shalazhashan of northern Alxa:Constraints on the southernmost boundary of the Central Asian Orogenic Belt[J]. Lithos, 201, 208~209:158~177.

    Google Scholar

    [36] 刘晔. 内蒙古东升庙-带花岗质片麻岩及侵入岩的地球化学、年代学特征及其构造意义[D]. 兰州: 兰州大学, 2012.http://cdmd.cnki.com.cn/Article/CDMD-10730-1012375117.htm

    Google Scholar

    LIU Ye. Geochemical and chronological characteristicsof the granitic gneisses and intrusive rocks in Dongshengmiao region, Inner Mongolia and their tectonic implications[D]. Lanzhou:Lanzhou University, 2012.

    Google Scholar

    [37] Hu J M, Gong W B, Wu S J, et al. LA-ICP-MS zircon U-Pb dating of the Langshan Group in the northeast margin of the Alxa block, with tectonic implications[J]. Precambrian Research, 2014, 255:756~770. doi: 10.1016/j.precamres.2014.08.013

    CrossRef Google Scholar

    [38] 彭润民, 翟裕生, 王建平, 等.内蒙狼山新元古代酸性火山岩的发现及其地质意义[J].科学通报, 2010, 55(26):2611~2620.

    Google Scholar

    PENG Run-min, ZHAI Yu-sheng, WANG Jian-ping, et al. Discovery of Neoproterozoic acid volcanic rock in the south-western section of Langshan, Inner Mongolia[J]. Chinese Science Bulletin (Chinese Version), 2010, 55(26):2611~2620.

    Google Scholar

    [39] 赵勇, 蔡向民, 李亚林, 等.内蒙古宝音图晚二叠世-晚三叠世花岗岩岩石化学特征及其构造环境[J].矿物岩石, 2011, 31(1):49~55.

    Google Scholar

    ZHAO Yong, CAI Xiang-min, LI Ya-lin, et al. The petrochemical characteristics and tectonic setting of the Late Permian and the Late Triassic for the granitic batholith in Buyant area, Inner Mongolia[J]. Journal of Mineralogy and Petrology, 2011, 31(1):49~55.

    Google Scholar

    [40] 皮桥辉, 刘长征, 陈岳龙, 等.内蒙古霍各乞海西期侵入岩形成时代、成因及其与铜矿体的关系[J].矿床地质, 2010, 29(3):437~451.

    Google Scholar

    PI Qiao-hui, LIU Chang-zheng, CHEN Yue-long, et al. Formation epoch and genesis of intrusive rocks in Huogeqi orefield of Inner Mongolia and their relationship with copper mineralization[J]. Mineral Deposits, 2010, 29(3):437~451.

    Google Scholar

    [41] 李怀坤, 朱士兴, 相振群, 等.北京延庆高于庄组凝灰岩的锆石U-Pb定年研究及其对华北北部中元古界划分新方案的进一步约束[J].岩石学报, 2010, 26(7):2131~2140.

    Google Scholar

    LI Huai-kun, ZHU Shi-xing, XIANG Zhen-qun, et al. Zircon U-Pb dating on tuffbed from Gaoyuzhuang formation in Yanqing, Beijing:Further constraints on the new subdivision of the Mesoproterozoic stratigraphy in the northern North China Craton[J]. Acta Petrologica Sinica, 2010, 26(7):2131~2140.

    Google Scholar

    [42] Liu Y S, Gao S, Hu Z C, et al. Continental and oceanic crust recycling-induced melt-peridotite interactions in the trans-North China Orogen:U-Pb dating, Hf isotopes and trace elements in zircons from mantle xenoliths[J]. Journal of Petrology, 2010, 51(1/2):537~571.

    Google Scholar

    [43] Ludwig KR. Isoplot/Ex:A Geochronological toolkit for microsoftexcel version 3.00[M]. Berkeley:Berkeley Geochronology Center, 2003, 4:1~70.

    Google Scholar

    [44] 耿建珍, 李怀坤, 张健, 等.锆石Hf同位素组成的LA-MC-ICP-MS测定[J].地质通报, 2011, 30(10):1508-1513. doi: 10.3969/j.issn.1671-2552.2011.10.004

    CrossRef Google Scholar

    GENG Jian-zhen, LI Huai-kun, ZHANG Jian, et al. Zircon Hf isotope analysis by means of LA-MC-ICP-MS[J]. Geological Bulletin of China, 2011, 30(10):1508~1513. doi: 10.3969/j.issn.1671-2552.2011.10.004

    CrossRef Google Scholar

    [45] Wu F Y, Yang Y H, Xie L W, et al. Hf isotopic compositions of the standard zircons and baddeleyites used in U-Pb geochronology[J]. Chemical Geology, 2006, 234(1/2):105~126.

    Google Scholar

    [46] Woodhead J, Hergt J, Shelley M, et al. Zircon Hf-isotope analysis with an excimer laser, depth profiling, ablation of complex geometries, and concomitant age estimation[J]. Chemical Geology, 2004, 209(1/2):121~135.

    Google Scholar

    [47] 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.

    Google Scholar

    [48] Griffin W L, Pearson N J, Belousova E, et al. The Hf isotope composition of cratonic mantle:LAM-MC-ICPMS analysis of zircon megacrysts in kimberlites[J]. Geochimica et Cosmochimica Acta, 2000, 64(1):133~147. doi: 10.1016/S0016-7037(99)00343-9

    CrossRef Google Scholar

    [49] Maniar P D, Piccoli P M. Tectonic discrimination of granitoids[J]. GSA Bulletin, 1989, 101(5):635~643. doi: 10.1130/0016-7606(1989)101<0635:TDOG>2.3.CO;2

    CrossRef Google Scholar

    [50] Peccerillo A, Taylor S R. Geochemistry of eocene calc-alkaline volcanic rocks from the Kastamonu area, Northern Turkey[J]. Contributions to Mineralogy and Petrology, 1976, 58(1):63~81. doi: 10.1007/BF00384745

    CrossRef Google Scholar

    [51] Sun S S, McDonough W F. Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes[A].Saunders A D, Norry M J. Magmatism in the Ocean Basin[M].Geological Society, London, Special Publications, 1989, 42(1):313~345.

    Google Scholar

    [52] 李献华, 李武显, 李正祥.再论南岭燕山早期花岗岩的成因类型与构造意义[J].科学通报, 2007, 52(9):981~991.

    Google Scholar

    LI Xian-hua, LI Wu-xian, LI Zheng-xiang. On the genetic classification and tectonic implications of the Early Yanshanian granitoids in the Nanling Range, South China[J]. Chinese Science Bulletin, 2007, 52(14):1873~1885.

    Google Scholar

    [53] Yang J H, Wu F Y, Shao J A, et al. Constraints on the timing of uplift of the Yanshan Fold and Thrust Belt, North China[J]. Earth and Planetary Science Letters, 2006, 246(3/4):336~352.

    Google Scholar

    [54] Pearce J A, Harris N B W, Tindle A G. Trace element discrimination diagrams for the tectonic interpretation of granitic rocks[J]. Journal of Petrology, 1984, 25(4):956~983. doi: 10.1093/petrology/25.4.956

    CrossRef Google Scholar

    [55] Barbarin B. A review of the relationships between granitoid types, their origins and their geodynamic environments[J]. Lithos, 1999, 46(3):605~626. doi: 10.1016/S0024-4937(98)00085-1

    CrossRef Google Scholar

    [56] Barbarin B. Granitoids:Main petrogenetic classifications in relation to origin and tectonic setting[J]. Geological Journal, 1990, 25(3/4):227~238.

    Google Scholar

    [57] Harris N B W, Pearce J A, Tindle A G. Geochemical characteristics of collision-zone magmatism[A]. Coward MP, Ries AC. Collision tectonics[M].Geological Society, London, Special Publications, 1986, 19(1):67~81.

    Google Scholar

    [58] 程裕淇.中国区域地质概论[M].北京:地质出版社, 1994.

    Google Scholar

    CHENG Yu-qi. Regional geological survey China[M]. Beijing:Geological Publishing House, 1994.

    Google Scholar

    [59] 张招崇, 王永强.冀北印支期碱性岩浆活动及其地球动力学意义[J].矿物岩石地球化学通报, 1997, 16(4):214~217.

    Google Scholar

    ZHANG Zhao-chong, WANG Yong-qiang. Indosinian alkaline magmatism in North Hebei Province and its geodynamic significance[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 1997, 16(4):214~217.

    Google Scholar

    [60] 柳长峰, 刘文灿, 周志广.内蒙古四子王旗地区古生代-早中生代侵入岩活动期次、特征及构造背景[J].地质学报, 2014, 88(6):992~1002.

    Google Scholar

    LIU Chang-feng, LIU Wen-can, ZHOU Zhi-guang. Geochronology, geochemistry and tectonic setting of the Paleozoic-Early Mesozoic intrusive in Siziwangqi, Inner Mongolia[J]. Acta Geologica Sinica, 2014, 88(6):992~1002.

    Google Scholar

    [61] 张维, 简平.华北北缘固阳二叠纪闪长岩-石英闪长岩-英云闪长岩套SHRIMP年代学[J].中国地质, 2012, 39(6):1593~1603.

    Google Scholar

    ZHANG Wei, JIAN Ping. SHRIMP dating of the Permian Guyang diorite-quartz diorite-tonalite suite in the northern margin of the North China Craton[J]. Geology in China, 2012, 39(6):1593~1603.

    Google Scholar

    [62] Yu Q, Ge W C, Zhang J, et al. Geochronology, petrogenesis and tectonic implication of Late Paleozoic volcanic rocks from the Dashizhai Formation in Inner Mongolia, NE China[J]. Gondwana Research, 2017, 43:164~177. doi: 10.1016/j.gr.2016.01.010

    CrossRef Google Scholar

    [63] 尚庆华.北方造山带内蒙古中、东部地区二叠纪放射虫的发现及意义[J].科学通报, 2004, 49(24):2574~2579.

    Google Scholar

    SHANG Qing-hua. Occurrences of Permian radiolarians in central and eastern Nei Mongol (Inner Mongolia) and their geological significance to the Northern China Orogen[J]. Chinese Science Bulletin, 2004, 49(24):2613~2619.

    Google Scholar

    [64] 王玉净, 樊志勇.内蒙古西拉木伦河北部蛇绿岩带中二叠纪放射虫的发现及其地质意义[J].古生物学报, 1997, 36(1):58~69.

    Google Scholar

    WANG Yu-jing, FAN Zhi-yong. Discovery of Permian radiolarians in ophiolite belt on northern side of XAR Moron River, Nei Monggol and its geological significance[J]. Acta Palaeontologica Sinica, 1997, 36(1):58~69.

    Google Scholar

    [65] 樊志勇.内蒙古西拉木伦河北岸杏树洼一带石炭纪洋壳"残片"的发现及其构造意义[J].中国区域地质, 1996, 15(4):382.

    Google Scholar

    FAN Zhi-yong. Discovery of the carboniferous oceanic crust fragments and its tectonic in the north of the Xila Mu River, Inner Mongolia[J]. Regional Geology of China, 1996, 15(4):382.

    Google Scholar

    [66] 任荣, 牟保磊, 韩宝福, 等.河北矾山钾质碱性超镁铁岩-正长岩杂岩体的锆石SHRIMP U-Pb年龄[J].岩石学报, 2009, 25(3):588~594.

    Google Scholar

    REN Rong, MU Bao-lei, HAN Bao-fu, et al. ZirconSHRIMP U-Pb dating of the Fanshan potassic alkaline ultramafite-syenite complex in Hebei Province, China[J]. Acta Petrologica Sinica, 2009, 25(3):588~594.

    Google Scholar

    [67] 吴福元, 徐义刚, 高山, 等.华北岩石圈减薄与克拉通破坏研究的主要学术争论[J].岩石学报, 2008, 24(6):1145~1174.

    Google Scholar

    WU Fu-yuan, XU Yi-gang, GAO Shan, et al. Lithospheric thinning and destruction of the North China Craton[J]. Acta Petrologica Sinica, 2008, 24(6):1145~1174.

    Google Scholar

    [68] 吕林素, 毛景文, 刘珺, 等.华北克拉通北缘岩浆Ni-Cu-(PGE)硫化物矿床地质特征、形成时代及其地球动力学背景[J].地球学报, 2007, 28(2):148~166.

    Google Scholar

    LV Lin-su, MAO Jing-wen, LIU Jun, et al. Geological characteristics, geochronology and tectonic settings of typical magmatic Ni-Cu-(PGE) sulfide deposits in thenorthern margin of the North China Craton[J]. Acta Geoscientica Sinica, 2007, 28(2):148~166.

    Google Scholar

    [69] 田伟, 陈斌, 刘超群, 等.冀北小张家口超基性岩体的锆石U-Pb年龄和Hf同位素组成[J].岩石学报, 2007, 23(3):583~590.

    Google Scholar

    TIAN Wei, CHEN Bin, LIU Chao-qun, et al. Zircon U-Pb age and Hf isotopic composition of the Xiaozhangjiakou ultramafic pluton in northern Hebei[J]. Acta Petrologica Sinica, 2007, 23(3):583~590.

    Google Scholar

    [70] 韩宝福, 加加美宽雄, 李惠民.河北平泉光头山碱性花岗岩的时代、Nd-Sr同位素特征及其对华北早中生代壳幔相互作用的意义[J].岩石学报, 2004, 20(6):74~87.

    Google Scholar

    HAN Bao-fu, Kagami H, LI Hui-min. Age and Nd-Sr isotopic geochemistry of the Guangtoushan alkaline granite, Hebei province, China:Implications for early Mesozoic crust-mantle interaction in North China Block[J]. Acta Petrologica Sinica, 2004, 20(6):74~87.

    Google Scholar

    [71] 牟保磊, 邵济安, 储著银, 等.河北矾山钾质碱性超镁铁岩-正长岩杂岩体Sm-Nd年龄和Sr、Nd同位素特征[J].岩石学报, 2001, 17(3):358~365.

    Google Scholar

    MU Bao-lei, SHAO Ji-an, CHU Zhu-yin, et al. Sm-Nd age and Sr, Nd isotopic characteristics of the Fanshan potassic alkaline ultramafite-syenite complex in Hebei province, China[J]. Acta Petrologica Sinica, 2001, 17(3):358~365.

    Google Scholar

    • Relative Articles
  • Cited by
  • Supplements
    • Proportional views
  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Figures(10)

Tables(3)

Export Citation
PDF
XML

Article Metrics

Article views(513) PDF downloads(4) Cited by(0)

Access History

Other Articles By Authors

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    版权所有：中国地质调查局发展研究中心 copyright @2020