吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (5): 1599-1614.doi: 10.13278/j.cnki.jjuese.20200011

• 整装勘查区矿床成因与成矿作用研究专辑 • 上一篇    

内蒙古西乌旗迪彦庙蛇绿岩带内辉长岩地球化学及年代学

熊光强1,2, 刘敏3, 张达1, 王忠4   

  1. 1. 江西省地质矿产勘查开发局物化探大队, 南昌 330025;
    2. 中国地质大学(北京)地球科学与资源学院, 北京 100083;
    3. 西北大学地质学系, 西安 710069;
    4. 内蒙古自治区地质调查院, 呼和浩特 010020
  • 收稿日期:2020-01-13 出版日期:2020-09-26 发布日期:2020-09-29
  • 通讯作者: 张达(1967-),教授,主要从事构造地质学及区域成矿规律研究,E-mail:zhangda@cugb.edu.cn E-mail:zhangda@cugb.edu.cn
  • 作者简介:熊光强(1988-),男,工程师,硕士,主要从事构造地质学研究,E-mail:xgq_1201@163.com
  • 基金资助:
    中国地质调查局项目（1212011085490，1212011120700）

Geochemistry and Geochronology of Gabbro in Diyanmiao Ophiolite Belt, West Ujimqin Banner, Inner Mongolia

Xiong Guangqiang1,2, Liu Min3, Zhang Da1, Wang Zhong4   

  1. 1. Geophysical and Geochemical Exploration Party, Jiangxi Bureau of Geology and Mineral Resources, Nanchang 330025, China;
    2. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China;
    3. Department of Geology, Northwest University, Xi'an 710069, China;
    4. Institute of Geological Survey of Inner Mongolia, Hohhot 010020, China
  • Received:2020-01-13 Online:2020-09-26 Published:2020-09-29
  • Supported by:
    Supported by Project of China Geological Survey (1212011085490, 1212011120700)

PDF (PC)

266

摘要： 内蒙古西乌旗迪彦庙蛇绿岩位于二连浩特—贺根山蛇绿岩带与交其尔—锡林浩特蛇绿岩带一线之间，大地构造位于中亚造山带中段的锡林浩特晚古生代褶皱带。本文主要对其内的辉长岩进行了地球化学及年代学研究。研究结果表明：辉长岩w（SiO2）为45.49%~50.48%，w（Al2O3）为13.31%~17.05%，w（K2O）为0.01%~0.65%，w（Na2O）为0.30%~4.15%，w（CaO）为8.00%~19.54%，w（MgO）为5.22%~10.92%，w（P2O5）为0.03%~0.23%，显示西乌旗迪彦庙蛇绿岩中的辉长岩属于高铝、低钾、低钠的拉斑系列；辉长岩的稀土元素总量低，重稀土元素比轻稀土元素富集，微量元素Nb、Zr、Hf、Ti相对亏损，K、Ta、Sr相对富集；La-ICP-MS锆石U-Pb测年获得辉长岩的年龄为（345.3±2.3）Ma，为早石炭世。综合分析，辉长岩可能为受到俯冲作用产生的流体交代而成，而并非结晶分异作用所致；迪彦庙蛇绿岩形成环境为弧前环境。

关键词: 迪彦庙, 地球化学, 锆石U-Pb定年, 蛇绿岩, 辉长岩

Abstract: The Diyanmiao ophiolite in the west Ujimqin Banner, Inner Mongolia, which tectonically belongs to the Xilinhaote Late Paleozoic fold belt in the southeastern Central Asian orogenic belt, is located between the Erlianhot-Hegenshan ophiolite belt and the Jiaoqier-Xilinhaote ophiolite belt. This study focuses on the geochemical and geochronological characteristics of the gabbros from the Diyanmiao ophiolite. Whole-rock geochemical data show that the gabbros are high Al, lower K, lower Na, and tholeiitic in nature, with w(SiO2) of 45.49%~50.48%, w(Al2O3) of 13.31%~17.05%, w(K2O) of 0.01%~0.65%, w(Na2O) of 0.30%~4.15%, w(CaO) of 8.00%~19.54%, w(MgO) of 5.22%~10.92%, and w(P2O5) of 0.03%~0.23%. These rocks have low total REE contents and relatively enriched HREE. They also show enrichments in K, Ta, and Sr, and depletions in Nb, Zr, Hf, and Ti. La-ICP-MS zircon U-Pb dating results suggest that the gabbros were formed at Early Carboniferous ((345.3±2.3) Ma). In combination with previously works and regional geology, the authors propose that the gabbros in the Diyanmiao ophiolite were possibly formed by fluids metasomatism in an island arc setting during oceanic subduction, rather than crystallization and differentiation processes.

Key words: Diyanmiao, geochemistry, zircon U-Pb dating, ophiolite, gabbro

中图分类号: 

  • P588.12
[1] Coleman R G. Ophiolites[M]. New York:Springer-Verlag, 1977:1-229.
[2] Steinmannn G. Die Ophiolitischen Zonen in den Mediterranean Kettengebirgen (The Ophiolitic Zones in the Mediterranean Mountain Chains)[J]. Translated by Daniel B, Gerald M F. Geological Society of America Special Paper, 2003, 373:77-91.
[3] 张旗. 蛇绿岩的分类[J]. 地质科学, 1990, 25(1):54-61. Zhang Qi. Classification of Ophiolites[J].Chinese Journal of Geology, 1990, 25(1):54-61.
[4] 臧遇时, 杨高学, 赵金凤. 蛇绿岩的定义、分类及其发展[J]. 西北地质, 2013, 46(2):12-17. Zang Yushi, Yang Gaoxue, Zhao Jinfeng. The Definition Classification and Development of Ophiolites[J]. Northwestern Geology, 2013, 46(2):12-17.
[5] Miyashiro A. The Troodos Complex Was Probably Formed in an Island Arc[J]. Earth Planetary Science Letters, 1973, 19:218-224.
[6] Pearce J A. Basalt Geochemistry Used to Investigate Past Tectonic Environments on Cyprus[J]. Tectonophysics, 1975, 25(1/2):41-67.
[7] Church W R, Riccio L. Fractionation Trend of the Bay of Islands Ophiolite of Newfoundland:Polycyclic Cumulate Sequences in Ophiolites and Their Classification[J]. Canadian Earth Sciences, 1977, 14(5):1156-1165.
[8] Moores E M. Origin and Emplacement of Ophiolites[J]. Reviews of Geophysics and Space Physics, 1982, 20(4):735-760.
[9] Coleman R G. The Diversity of Ophiolites[J]. Geologicen Mijnbouw, 1984, 63(2):144-150.
[10] Boudier F, Nicolas A. Harzburgite and Lherzolite Subtypes in Ophiolitic and Oceanic Environments[J]. Earth and Planetary Science Letters, 1985, 76(1/2):84-92.
[11] 朱宝清, 王来生, 王连晓. 西准噶尔西南地区古生代蛇绿岩[J]. 中国地质科学院西安地质矿产研究所所刊, 1987, 17:3-64. Zhu Baoqing, Wang Laisheng, Wang Lianxiao.Paleozoic Ophiolite in Southwest of Western Junggar[J]. Bulletin of the Xi'an Institute of Geology and Mineral Resources, the Chinese Academy of Geologica Sciences, 1987, 17:3-64.
[12] 王希斌, 鲍佩声. 中国大陆造山带中地幔橄榄岩体的熔融残余类型及其构造形变[J]. 地球学报, 1990, 11(1):49-52. Wang Xibin, Bao Peisheng. Types of Melting Residue and Structural Deformation of the Mantle Peridotite Bodies in Orogenic Belts of China[J]. Axta Geoscienca Sinica, 1990, 11(1):49-52.
[13] 王希斌, 鲍佩声, 戎合. 中国蛇绿岩中变质橄榄岩的稀土元素地球化学[J]. 岩石学报, 1995, 11(增刊1):24-41. Wang Xibin, Bao Peisheng, Rong He. Rare Earth Elements Geochemistry of the Mantle Peridotite in the Ophiolite Suites of China[J]. Acta Petrologica Sinica, 1995, 11(Sup. l):24-41.
[14] 肖序常. 从扩张速率试论蛇绿岩的类型划分[J]. 岩石学报, 1995, 11(增刊1):10-23. Xiao Xuchang. Discussion on the Classification of Ophiolites by Spreading Rate[J]. Acta Petrologica Sinica, 1995, 11(Sup. l):10-23.
[15] Dilek Y, Furnes H. Ophiolite Genesis and Global Tectonics:Geochemical and Tectonic Fingerprinting of Ancient Oceanic Lithosphere[J]. Geological Society of America Bulletin, 2011, 123(3/4):387-411.
[16] 张旗, 周国庆, 王焰. 中国蛇绿岩的分布、时代及其形成环境[J]. 岩石学报, 2003, 19(1):1-8. Zhang Qi, Zhou Guoqing, Wang Yan. The Distribution of Time and Space of Chinese Ophiolites, and Their Tectonic Settings[J]. Acta Petrologica Sinica, 2003, 19(1):1-8.
[17] 梁日喧. 内蒙古中段蛇绿岩特征及地质意义[J]. 中国区域地质,1994, 1:37-45. Liang Rixuan. The Features of Ophiolites in the Gentral Sector of Inner Mongolia and Its Ecological Significance[J]. Regional Geology of China, 1994, 1:37-45.
[18] Hsu K J, Wang Q, Hao J. Geologic Evolution of the Neomonides:A Working Hypothesis[J].Eclogae Geologicae Helvetiae, 1991, 84(1):1-31.
[19] Şengör A M C, Natalin B A, Burtman V S. Evolution of the Altaid Tectonic Collage and Paleozoic Crustal Growth in Eurasia[J]. Nature, 1993, 364:299-307.
[20] 包志伟, 陈森煌, 张桢堂. 内蒙古贺根山地区蛇绿岩稀土元素和Sr-Nd同位素研究[J]. 地球化学, 1994, 23(4):339-349. Bao Zhiwei, Chen Senhuang, Zhang Zhentang. Study on Ree and Sm-Nd Isotopes of Hegenshan Ophiolite, Inner Mongolia[J]. Geochimica, 1994, 23(4):339-349.
[21] Miao L C, Fan W M, Liu D Y, et al. Geochronology and Geochemistry of the Hegenshan Ophiolitic Complex:Implications for Late-Stage Tectonic Evolution of the Inner Mongolia-Daxinganling Orogenic Belt, China[J]. Journal of Asian Earth Sciences, 2008, 32(5/6):348-370.
[22] Tang K D. Tectonic Development of the Paleozoic Foldbelts at the Northern Margin of the Sino-Korean Craton[J]. Tectonics, 1990, 9(2):249-260.
[23] 唐克东. 中朝板块北侧褶皱带构造演化及成矿规律[M]. 北京:北京大学出版社, 1992. Tang Kedong. Tectonic Evolution and Metallogenic Regularity of the Fold Belt in the North and North China Plate[M]. Beijing:Peking University Press, 1992.
[24] 陈斌, 徐备. 内蒙古苏尼特左旗地区古生代两类花岗岩类的基本特征和构造意义[J]. 岩石学报, 1996, 12(4):546-561. Chen Bin, Xu Bei. The Main Characteristics and Tectonic Implications of Two Kinds of Paleozoic Granitoids in Sunidzuqi, Central Inner Mongolia[J]. Acta Petrologica Sinica, 1996, 12(4):546-561.
[25] 郝旭, 徐备. 内蒙古锡林郭勒杂岩的原岩年代和变质年代[J]. 地质论评, 1997, 43(1):101-105. Hao Xu, Xu Bei. Sm-Nd, Rb-SrIsotopic Geochronology of the Xilin Gol Complex, Inner Mongolia, China[J]. Geological Review, 1997, 43(1):101-105.
[26] Chen B, Jahn B, Wilde S, et al. Two Contrasting Paleosoic Magmatic Belts in Northern Inner Mongolia, China:Petrogenesis and Tectonic Implications[J]. Tectonophysics, 2000, 328(1/2):157-182.
[27] 黄金香, 赵志丹, 张宏飞, 等. 内蒙古温都尔庙和巴彦敖包-交其尔蛇绿岩的元素与同位素地球化学:对古亚洲洋东部地幔域特征的限制[J]. 岩石学报, 2006, 22(12):2889-2900. Huang Jinxiang, Zhao Zhidan, Zhang Hongfei, et al. Elemental and Sr-Nd-Pb Isotopic Geochemistry of the Wenduermiao and Bayanaobao-Jiaoqier Ophiolites, Inner Mongolia:Constraints for the Characteristics of the Mantle Domain of Eastern Paleo-Asian Ocean[J]. Acta Petrologica Sinica, 2006, 22(12):2889-2900.
[28] 陶继雄, 苏茂荣, 宝音乌力吉, 等. 内蒙古达尔罕茂明安联合旗满都拉地区索伦山蛇绿混杂岩的特征及构造意义[J]. 地质通报, 2004, 23(12):1238-1242. Tao Jixiong, Su Maorong,Baoyin Wuliji, et al. Characteristics and Tectonic Significance of the Sonol Mountain Ophiolitic Mélang in the Mandula Area, Darhan Muminggan, Inner Mongolia[J]. Geological Bulletn of China, 2004, 23(12):1238-1242.
[29] 王荃, 刘雪亚, 李锦轶. 中国华夏与安加拉古陆间的板块构造[M]. 北京:北京大学出版社, 1991. Wang Quan, Liu Xueya, Li Jinyi. Plate Tectonic Between Cathaysia and Angara[M]. Beijing:Peking University Press, 1991.
[30] 邵济安.内蒙古中部早古生代蛇绿岩及其在恢复地壳演化历史中的意义[C]//《中国北方板块构造论文集》编委会.中国北方板块构造论文集:第一集.北京:地质出版社,1986:158-172. Shao Ji'an. The Early Protozoic Ophiolite in Middle Inner Mongolia and Its Implications for Reconstruct Crust Evolution[C]//CPPTNC Editorial Committee. Contributions to the Project of Plate Tectonics in Northern China:No 1. Beijing:Geological Publishing House, 1986:158-172.
[31] 邵济安. 中朝板块北缘中段地壳演化[M]. 北京:北京大学出版社, 1991. Shao Ji'an. Crust Evolution in the Middle Part of the Northern Margin of Sion-Korean Plate[M]. Beijing:Peking University Press, 1991.
[32] 王东方. 内蒙古温都尔庙地区古板块会聚带的岩石化学和地球化学[J]. 北京大学学报(自然科学版), 1986, 27(2):111-123. Wang Dongfang. The Petrology and Geochemistry of Convergent Zone of Old Plate at the Ondor Sum District, Neimongol[J]. Acta Scientiarum Naturaliun Universitatis Pekinensis, 1986, 27(2):111-123.
[33] 许传诗. 内蒙古温都尔庙地区蛇绿岩变质作用的研究[J]. 河北地质学院学报, 1987, 10(1):1-26. Xu Chuanshi. On the Metamorphism of Wenduermiao Ophiolite, Inner Mongolia[J]. Journal of Hebei College of Geology, 1987, 10(1):1-26.
[34] 许传诗. 内蒙古温都尔庙地区蛇绿岩微量元素特征及其岩石学成因意义[J]. 河北地质学院学报, 1990, 13(1):1-8. Xu Chuanshi. Features of Trace Elements of Ophiolites in Wenduermiao Area, Nei Mongol and Their Significance in Rock Genesis[J]. Journal of Hebei College of Geology, 1990, 13(1):1-8.
[35] 牛树银, 胡晓, 孙爱群. 华北地台北侧的古板块构造演化[J]. 地质科技情报, 1993, 12(1):17-21. Niu Shuyin, Hu Xiao, Sun Aiqun. Evolution of the Paleoplate Tectonics on North Side of North China Platform[J]. Geological Science and Technology Information, 1993, 12(1):17-21.
[36] 刘敦一, 简平, 张旗, 等. 内蒙古图林凯蛇绿岩中埃达克岩SHRIMP测年:早古生代洋壳消减的证据[J]. 地质学报, 2003, 77(3):317-330. Liu Dunyi, Jian Ping, Zhang Qi, et al. SHRIMP Dating of Adakites in the Tulinkai Ophiolite, Inner Mongolia:Evidence for the Early Paleozoic Subduction[J]. Acta Geologica Sinica, 2003, 77(3):317-330.
[37] 李英杰, 王金芳, 李红阳, 等. 内蒙古西乌珠穆沁旗迪彦庙蛇绿岩的识别[J]. 岩石学报, 2012, 28(4):1282-1290. Li Yingjie, Wang Jinfang, Li Hongyang, et al. Recognition Diyanmiao Ophiolite in Xi Ujimqin Banner, Inner Mongolia[J]. Acta Petrologica Sinica, 2012, 28(4):1282-1290.
[38] 唐克东, 张允平. 内蒙古缝合带的构造演化[M]. 北京:北京科学技术出版社, 1991. Tang Kedong, Zhang Yunping.Tectonic Evolution of Suture Zone in Inner Mongolia[M]. Beijing:Beijing Science and Technology Press, 1991.
[39] Black L P, Kamo S L, Allen C M, et al. Improved 206Pb/238U Microprobe Geochronology by the Monitoring of a Trace-Element-Related Matrix Effect; SHRIMP, ID-TIMS, ELA-ICP-MS and Oxygen Isotope Documentation for a Series of Zircon Standards[J]. Chemical Geology, 2004, 205(1/2):115-140.
[40] 李怀坤, 陆松年, 李惠民, 等. 侵入下马岭组的基性岩床的锆石和斜锆石U-Pb精确定年:对华北中元古界地层划分方案的制约[J]. 地质通报, 2009, 28(10):1396-1404. Li Huaikun, Lu Songnian, Li Huimin, et al. Zircon and Beddeleyite U-Pb Precision Dating of Basic Rock Sills Intruding Xiamaling Formation, North China[J]. Geological Bulletn of China, 2009, 28(10):1396-1404.
[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. Li Huaikun, Zhu Shixing, Xiang Zhenqun, 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.
[42] Jackson S E, Pearson N J, Griffin W J, et al. The Application of Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry to in Situ U-Pb Zircon Geochronology[J]. Chemical Geology, 2004, 211(1/2):47-69.
[43] Black L P, Kamo S L, Allen C M, et al. A New Zircon Standard for Phanerozoic U-Pb Geochronology[J]. Chemical Geology, 2003, 200(1/2):155-170.
[44] Liu Y S, Gao S, Hu Z C, et al. Continental and Oceanic Crust Recycline-Induced Melt-Peridotite Interactions in the Trans-North China Orengen:U-Pb Dating, Hf Isotopes and Trace Elements in Zircons from Mantle Xenoliths[J]. Journal of Petrology, 2009, 51(1/2):537-571.
[45] Ludwing K R. Users Manual for Isoplot/Ex:A Geochronological Toolkit for Microsoft Excel[J]. Berkeley Geochronology Centre Special Publication, 2001, 1a:1-55.
[46] Andersen T. Correction of Common Lead in U-Pb Analyses That do not Report 204Pb[J]. Chemical Geology, 2002, 192(1/2):59-79.
[47] 白卉, 张红晨, 贺秋利, 等. 内蒙古迪彦庙蛇绿岩辉长岩岩石学特征[J]. 地质与资源, 2012, 21(6):531-534. Bai Hui, Zhang Hongchen, He Qiuli, et al. Lithology of Gabbro of the Diyanmiao Ophiolite in Inner Mongolia[J]. Geology and Resources, 2012, 21(6):531-534.
[48] 邱家骧. 岩浆岩岩石学[M]. 北京:地质出版社, 1985. Qiu Jiaxiang. Magmatic Petrology[M]. Beijing:Geological Publishing House, 1985.
[49] 赵莉, 张招崇, 王福生, 等. 一个开放的岩浆房系统:攀西新街镁铁-超镁铁质层状岩体[J]. 岩石学报, 2006, 22(6):1565-1578. Zhao Li, Zhang Zhaochong, Wang Fusheng, et al. Open-System Magma Chamber:An Example from the Xinjie Mafic-Ultramafic Layered Intrusion in Panxi Region, SW China[J]. Acta Petrologica Sinica, 2006, 22(6):1565-1578.
[50] 张旗, 周国庆. 中国蛇绿岩[M]. 北京:科学出版社, 2001. Zhang Qi, Zhou Guoqing.Ophiolite in China[M]. Beijing:Science Press, 2001.
[51] 吴元保, 郑永飞. 锆石成因矿物学研究及其对U-Pb年龄解释的制约[J]. 科学通报, 2004, 49(16):1589-1604. Wu Yuanbao, Zheng Yongfei. The Study of Zircon Genesis Mineralogy and Constraints of the Interpretation on Its U-Pb Age[J]. Chinese Science Bulletin, 2004, 49(16):1589-1604.
[52] Keppler H. Constraints from Partitioning Experiments on the Composition of Subductoin-Zone Fluids[J]. Nature, 1996, 380:237-240.
[53] 孟繁聪, 薛怀民, 李天福, 等. 苏鲁造山带晚中生代地幔的富集特征:来自辉长岩的地球化学证据[J]. 岩石学报, 2005, 21(6):1583-1592. Meng Fancong, Xue Huaimin, Li Tianfu, et al. Enriched Characteristics of Late Mesozoic Mantke Under the Sulu Orogenic Belt:Geochemical Evidence from Gabbro in Rushan[J]. Acta Petrologica Sinica, 2005, 21(6):1583-1592.
[54] 周长勇, 吴福元, 葛文春, 等. 大兴安岭北部塔河堆晶辉长岩体的形成时代、地球化学特征及其成因[J]. 岩石学报, 2005, 21(3):763-775. Zhou Changyong, Wu Fuyuan, Ge Wenchun, et al. Age,Geochemistry and Petrogenesis of the Cumulate Gabbro in Tahe, Northern Da Hinggan Mountain[J]. Acta Petrologica Sinica, 2005, 21(3):763-775.
[55] 蔡克大, 袁超, 孙敏, 等. 阿尔泰塔尔浪地区斜长角闪岩和辉长岩的形成时代、地球化学特征和构造意义[J]. 岩石学报, 2007, 23(5):877-888. Cai Keda, Yuan Chao, Sun Min, et al. Geochemical Characteristics and Ages of the Amplibolites and Gabbors in Tarlang Area:Implications for Tectonic Evolution of the Chinese Altai[J]. Acta Petrologica Sinica, 2007, 23(5):877-888.
[56] Zhao Z H, Zhou L D. REE Geochemistry of Some Alkali-Rich Intrusive Rocks in China[J]. Science in China:Series D, 1997, 40(2):145-158.
[57] Jian P, Kröner A, Windley B F, et al. Carboniferous and Cretaceous Mafic-Ultramafic Massifs in Inner Mongolia (China):A SHRIMP Zircon and Geochemical Study of the Previously Presumed Integral "Hegenshan Ophiolite"[J]. Lithos, 2012, 142/143(2):48-66.
[58] Zhang Z C, Li K, Li J F, et al. Geochronology and Geochemistry of the Eastern Ophiolitic Complex:Implications for the Tectonic Evolution of the Inner Mongolia-Daxinganling Orogenic Belt[J]. Journal of Asian Earth Sciences, 2015, 97:279-293.
[59] 李英杰, 王金芳, 李红阳, 等. 内蒙古西乌旗梅劳特乌拉蛇绿岩的识别[J]. 岩石学报, 2015, 31(5):1461-1470. Li Yingjie, Wang Jinfang, Li Hongyang, et al.Recognition of Meilaotewula Ophiolite in Xi U jimqin Banner, Inner Mongolia[J]. Acta Petrologica Sinica, 2015, 31(5):1461-1470.
[60] Song S G, Wang M M, Xu X, et al. Ophiolites in the Xing'an-Inner Mongolia Accretionary Belt of the CAOB:Implications for Two Cycles of Seafloor Spreading and Accretionary Orogenic Events[J]. Tectonics, 2015, 34(10):2221-2248.
[61] 黄波, 付冬, 李树才, 等. 内蒙古贺根山蛇绿岩形成时代及构造启示[J]. 岩石学报, 2016, 32(1):158-176. Huang Bo, Fu Dong, Li Shucai, et al. The Age and Tectonic Implications of the Hegenshan Ophiolite in Inner Mongolia[J]. Acta Petrologica Sinica, 2016, 32(1):158-176.
[62] Yang J F, Zhang Z C, Chen Y, et al. Ages and Origin of Felsic Rocks from the Eastern Erenhot Ophiolitic Complex, Southeastern Centera Asian Orogenic Belt, Inner Mongolia China[J]. Journal of Asian Earth Sciences, 2017, 144(3/4):126-140.
[63] Li Y J, Wang G H, Santosh M, et al. Supra-Subduction Zone Ophiolites from Inner Mongolia, North China:Implications for the Tectonic History of the Southeaetern Central Asian Orogenic Belt[J]. Gondwana Research, 2018, 59(3):126-143.
[64] 李英杰, 王金芳, 王根厚, 等. 内蒙古迪彦庙蛇绿岩带达哈特前弧玄武岩的发现及其地质意义[J]. 岩石学报, 2018, 34(2):469-482. Li Yingjie, Wang Jinfang, Wang Genhou, et al. Discovery and Significance of the Dahate Fore-Arc Basalts from the Diyanmiao Ophiolite in Inner Mongolia[J]. Acta Petrologica Sinica, 2018, 34(2):469-482.
[65] 王金芳, 李英杰, 李红阳, 等. 贺根山缝合带白音呼舒奥长花岗岩锆石U-Pb年龄、地球化学特征及构造意义[J]. 地质论评, 2019, 65(4):857-872. Wang Jinfang, Li Yingjie, Li Hongyang, et al. Zircon U-Pb Ages and Geochemical Characteristics of Baiyinhushu Trondhjemite in Hegenshan Suture Zone and Their Tectonic Implications[J]. Geological Review, 2019, 65(4):857-872.
[66] 陈斌, 赵国春, Simon Wilde. 内蒙古苏尼特左旗南两类花岗岩同位素年代学及其构造意义[J]. 地质论评, 2001, 47(4):361-367. Chen Bin, Zhao Guochun, Simon Wilde.Subduction-and Collision-Related Granitoids from Southern Sonidzuoqi, Inner Mongolia:Isotopic Ages and Tectonic Implications[J]. Geological Review, 2001, 47(4):361-367.
[67] 鲍庆中, 张长捷, 吴之理, 等. 内蒙古白音高勒地区石炭纪石英闪长岩SHRIMP锆石U-Pb年代学及其意义[J]. 吉林大学学报(地球科学版), 2007, 37(1):15-23. Bao Qingzhong, Zhang Changjie, Wu Zhili, et al.SHRIMP U-Pb Zircon Geochronology of a Carboniferous Quartz-Diorite in Baiyingaole Area, Inner Mongolia and Its Implications[J]. Journal of Jilin University (Earth Science Edition), 2007, 37(1):15-23.
[68] 刘建峰, 迟效国, 张兴洲, 等. 内蒙古西乌旗南部石炭纪石英闪长岩地球化学特征及其构造意义[J]. 地质学报, 2009, 83(3):365-376. Liu Jianfeng, Chi Xiaoguo, Zhang Xingzhou, et al. Geochemical Characteristic of Carboniferous Quartz-Diorite in the Southern Xiwuqi Area, Inner Mongolia and Its Tectonic Significance[J]. Acta Geologeica Sinica, 2009, 83(3):365-376.
[69] 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.
[70] 张拴宏, 赵越, 刘建民, 等. 华北板块北缘晚古生代-早中古生代岩浆活动期次、特征及构造背景[J].岩石矿物学杂志, 2010, 29(6):824-842. Zhang Shuanhong, Zhao Yue, Liu Jianmin, et al. Geochronology,Geochemistry and Tectonic Setting of the Late Paleozoic-Early Mesozoic Magmatism in the Northern Margin of the North China Block:Apreliminary Review[J]. Acta Petrologica et Mineralogica, 2010, 29(6):824-842.
[71] Kidd R G W. A Model for the Process of Formation of the Upper Oceanic Crust[J]. Geophysical Journal International, 1977, 50(1):149-183.
[72] Pearce J A, Lippard S J, Roberts S. Characteristics and Tectonic Significance of Supra-Subduction Zone Ophiolites[J].Geolgical Society London Special Publications, 1984, 16(1):77-94.
[73] Robinson P T, Zhou M F, Hu X F, et al. Geochemical Constraints on the Origin of the Hengenshan Ophiolite, Inner Mongolia, China[J]. Journal of Asian Earth Sciences, 1999, 17(4):423-442.
[74] Nozaka T, Liu Y. Petrology of the Hegenshan Ophiolite and Its Implication for the Tectonic Evolution of Northern China[J]. Earth and Planetary Science Letters, 2002, 202(1):89-104.
[75] Dilek Y, Robinson P T. Ophiolites in Earth History:Introduction[C]//Dilek, Robinson P T. Ophiolites in Earth History. London:Geological Society, 2003:1-8.
[76] Dilek Y, Furnes H. Structure and Geochemistry of Tethyan Ophiolites and Their Petrogenesis in Subduction Rollback Systems[J]. Lithos, 2009, 113(1/2):1-20.
[77] Dilek Y, Furnes H. Ophiolites and Their Origins[J]. Elements, 2014, 10(2):93-100.
[78] Stern R J, Ali K A, Liegeois J P, et al. Distribution and Signify-Cance of Pre-Neoproterozoic Zircons Injuvenile Neoproterozoic Igneous Rocks of the Arabian-Nubianshield[J]. American Journal of Science, 2010, 310(9):791-811.
[79] Li J Y. Permian Geodynamic Setting of Northeast China and Adjacent Regions:Closure of the Paleo-Asian Ocean and Subduction of the Paleo-Pacific Plate[J]. Journal of Asian Earth Sciences, 2006, 26(3/4):207-224.
[80] 王树庆, 许继峰, 刘希军, 等. 内蒙朝克山蛇绿岩地球化学:洋内弧后盆地的产物?[J]. 岩石学报, 2008, 24(12):2869-2879. Wang Shuqing, Xu Jifeng, Liu Xijun, et al. Geochemistry of the Chaokeshan Ophiolite:Product of Intra-Oceanic Back-Arc Basin?[J]. Acta Petrologica Sinica,2008, 24(12):2869-2879.
[81] 周国庆. 蛇绿岩研究新进展及其定义和分类的再讨论[J]. 南京大学学报(自然科学版), 2008, 44(1):1-24. Zhou Guoqing. Ophiolite:Some Key Aspects Regarding Its Definition and Classification[J]. Journal of Nanjing University (Natural Sciences), 2008, 44(1):1-24.
[82] 王成,任利民,张晓军,等. 内蒙古崇根山蛇绿岩前弧玄武岩的发现及其地质意义[J].地质科技情报, 2019, 38(3):1-11. Wang Cheng, Ren Limin, Zhang Xiaojun, et al. Discovery and Significance of the Fore-Arc Basalts from the Chonggenshan Ophiolitein Inner Mongolia[J]. Geological Science and Technology Information, 2019, 38(3):1-11.
[1] 赵亚云, 刘晓峰, 刘远超, 次琼, 郑常云, 杨春四, 李莉, 付海龙. 西藏昂仁县多仁则—桑阿卡地区铜多金属矿点含矿岩体成因及成矿意义[J]. 吉林大学学报(地球科学版), 2020, 50(5): 1323-1339.
[2] 范媛媛, 刘云华, 于晓飞, 赵强, 李小严, 邓楠, 马塬皓. 甘肃武都金坑子金矿床地球化学特征及成因探讨[J]. 吉林大学学报(地球科学版), 2020, 50(5): 1404-1417.
[3] 孙海瑞, 吕志成, 于晓飞, 李永胜, 杜泽忠, 吕鑫, 公凡影. 甘肃柳园地区早二叠世正长花岗斑岩脉锆石U-Pb年代学、岩石地球化学特征——对北山造山带晚古生代构造背景的指示[J]. 吉林大学学报(地球科学版), 2020, 50(5): 1433-1449.
[4] 范飞鹏, 肖惠良, 陈乐柱, 李海立, 刘建雄, 邓中林, 康丛轩, 林耿伟, 陈凯. 粤东莲花山地区多期岩浆锆石年代学、Hf同位素组成及其成矿作用[J]. 吉林大学学报(地球科学版), 2020, 50(5): 1462-1490.
[5] 贺根文, 路思明, 彭琳琳, 于长琦, 李伟, 刘翠辉. 赣南狮吼山硫铁多金属矿区花岗岩地球化学、年代学特征及其成因[J]. 吉林大学学报(地球科学版), 2020, 50(5): 1491-1504.
[6] 余振东, 项新葵, 谭荣, 孙德明, 张斯. 赣北大湖塘平苗矿段白云母花岗岩锆石U-Pb年代学、地球化学及地质意义[J]. 吉林大学学报(地球科学版), 2020, 50(5): 1505-1517.
[7] 余长胜, 杨言辰, 韩世炯, 杨昆林, 宋朝阳, 张易航, 王旺. 大兴安岭下嘎来奥伊铅锌矿床钾长花岗岩的岩石成因及地质意义[J]. 吉林大学学报(地球科学版), 2020, 50(4): 1042-1058.
[8] 任文恺, 王生云, 陈礼标, 吴少锋, 张海青. 青海同仁兰采地区花岗闪长岩LA-ICP-MS锆石U-Pb年代学、地球化学特征及其地质意义[J]. 吉林大学学报(地球科学版), 2020, 50(4): 1059-1074.
[9] 王德远, 续海金, 王攀, 贾敏, 高占冬. 大陆造山带深熔垮塌的岩石学、地球化学证据:以北大别深熔混合岩为例[J]. 吉林大学学报(地球科学版), 2020, 50(3): 675-693.
[10] 任云生, 刘小禾, 商青青, 陈聪, 杨群, 郝宇杰, 孙振明. 吉林省和龙地区鸡南BIF型铁矿床含矿建造地球化学特征及形成时代[J]. 吉林大学学报(地球科学版), 2020, 50(3): 800-814.
[11] 张健, 张海华, 陈树旺, 郑月娟, 张德军, 苏飞, 黄欣. 松辽盆地北部上二叠统林西组地球化学特征及地质意义[J]. 吉林大学学报(地球科学版), 2020, 50(2): 518-530.
[12] 陈会军, 于宏斌, 马永非, 陈井胜, 钱程, 刘世伟, 崔天日, 钟辉. 吉东南地区五女峰岩体锆石U-Pb年代学、岩石地球化学特征及其构造意义[J]. 吉林大学学报(地球科学版), 2020, 50(2): 531-541.
[13] 孟庆涛, 李金国, 刘招君, 胡菲, 徐川. 茂名盆地羊角含矿区始新统油柑窝组油页岩有机地球化学特征及沉积环境[J]. 吉林大学学报(地球科学版), 2020, 50(2): 356-367.
[14] 宋宇, 刘招君, Achim Bechtel, 徐银波, 孟庆涛, 孙平昌, 朱凯. 老黑山盆地下白垩统穆棱组油页岩与煤含油率控制因素[J]. 吉林大学学报(地球科学版), 2020, 50(2): 378-391.
[15] 郑国栋, 孟庆涛, 刘招君. 松辽盆地北部青一段油页岩地球化学特征及其记录的古湖泊学信息[J]. 吉林大学学报(地球科学版), 2020, 50(2): 392-404.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
No Suggested Reading articles found!
版权所有 © 《吉林大学学报(地球科学版)》编辑部
地址：长春市西民主大街938号(130026)　电话：+86-431-88502374；13756165364　E-mail: xuebao1956@jlu.edu.cn
本系统由北京玛格泰克科技发展有限公司设计开发