China Geological Survey Chinese Academy of Geological SciencesHost
科学出版社Publish
Advanced Search
Previous Article Next Article
2020 Vol. 47, No. S1
Article Contents
Article navigation > Geology in China > 2020 > 47(S1): 40-49
Next Article Previous Article

REN Bangfang, DUAN Lianfeng, LI Min, NIU Wenchao, REN Yunwei. 2020. Geochronological and Geochemical Dataset of Late Paleozoic Granitoids in the Hazhu Area of Beishan, Inner Mongolia[J]. Geology in China, 47(S1): 40-49. doi: 10.12029/gc2020Z105
Citation: REN Bangfang, DUAN Lianfeng, LI Min, NIU Wenchao, REN Yunwei. 2020. Geochronological and Geochemical Dataset of Late Paleozoic Granitoids in the Hazhu Area of Beishan, Inner Mongolia[J]. Geology in China, 47(S1): 40-49. doi: 10.12029/gc2020Z105
shu

Geochronological and Geochemical Dataset of Late Paleozoic Granitoids in the Hazhu Area of Beishan, Inner Mongolia

    Fund Project: China Geological Survey Project (DD20160039, DD20190382)
More Information
  • Author Bio: REN Bangfang, male, born in 1981, senior engineer, mainly engages in research on basic geology and geochemistry; E-mail: bangfangren@foxmail.com
  • Corresponding author: NIU Wenchao, male, born in 1986, engineer, mainly engages in researches on the regional geological survey and orogenic belt; E–mail: billynu2003@163.com  
Received Date:  08 April 2020
Revised Date:  27 April 2020
Publish Date:  25 June 2020
    Abstract

  • Under the project of ‘1∶5 000 Regional Geological and Mineral Survey of the Hazhu, Hazhudongshan, Hazhunanshan and Lishitan Map-sheet’ by China Geological Survey, this dataset was compiled though rock analysis and tests based on detailed geological field surveys. This paper presents the test data of Late Paleozoic granite samples in the Hazhu area in Beishan, Inner Mongolia. The rock types include tonalite, granodiorite, monzonitic granite and alkaline feldspar granite. Zircon chronological data show that the formative era of these kind of rocks are Carboniferous–Permian. The whole-rock macroelement and trace element data show that Carboniferous granitoids are of the metaluminous-weak peraluminous and medium-K calc-alkaline series. The distribution curve of rare earth elements displays right-leaning characteristics. Trace elements are rich in large-ion lithophile elements including Rb, Ba and K; and deficient in high field-strength elements including Nb, Ta and Ti; thus, indicating that magma was formed in a continental marginal arc environment related to the subduction belt. In contrast, Permian granitoids display high-silicon, alkali-rich, metaluminous and magnesium-deficient features, and constitute a medium-high-K calc-alkaline series. They are also rich in large-ion lithophile elements and deficient in high-field strength elements. However, graphic texture is developed within alkaline feldspar granite and crystal caves are developed on a large scale in granodiorite, indicating that the Permian rock mass is situated in an extensional environment. The combination of the two can provide a basis and fundamental data support for studying the subduction polarity and tectonic evolution of the Hongshishan–Baiheshan Ocean in the Beishan area. This dataset is presented in the form of Excel tables, including two. xls files (Geochemistry data_HZ. Xls and Zircon U–Pb dating data_HZ. xls), which record the 27 samples’ geochemical data and 11 samples’ zircon U–Pb dating results of the samples, respectively. The samples of this dataset were all tested at the Tianjin Center laboratory of China Geological Survey, with reliable data quality.

    • FullText(HTML)
  • 加载中
    • References
  • [1] Andersen T. 2002. Correction of common lead in U-Pb analyses that do not report 204Pb[J]. Chemical Geology, 192: 59−79. doi: 10.1016/S0009-2541(02)00195-X

    CrossRef Google Scholar

    [2] Jackson Simon E, Pearson Norman J, Griffin William L, Belousova Elena A. 2004. The application of laser ablation-inductively coupled plasma-mass spectrometry to in situ U–Pb zircon geochronology[J]. Chemical Geology, 211: 47–69.

    Google Scholar

    [3] Liu YS, Gao S, Hu ZC, Gao CG, Zong KQ, Wang DB. 2010. 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, 51(1–2): 537−571. doi: 10.1093/petrology/egp082

    CrossRef Google Scholar

    [4] Ludwig KR. 2003. Isoplot/Ex Version 3.00: A Geochronological Toolkit for Microsoft Excel[J]. Berkeley Geochronology Center Special Publication, 4: 1−70.

    Google Scholar

    [5] Whitney DL, Evans BW. 2010. Abbreviations for names of rock-forming minerals[J]. American Mineralogist, 95: 185−187. doi: 10.2138/am.2010.3371

    CrossRef Google Scholar

    [6] Xiao WJ, Mao QG, Windley BF, Han CM, Qu JF, Zhang JE, Ao SJ, Guo QQ, Cleven NR, Lin SF, Shan YH, Li JL. 2010. Paleozoic multiple accretionary and collisional processes of the Beishan orogenic collage[J]. American Journal of Science, 310(10): 1553−1594. doi: 10.2475/10.2010.12

    CrossRef Google Scholar

    [7] Yuan HL, Gao S, Liu XM, Li HM, Detlef G, Wu FY. 2004. Accurate U-Pb Age and Trace Element Determinations of Zircon by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry[J]. Geostandards and Geoanalytical Research, 28(3): 353−370. doi: 10.1111/j.1751-908X.2004.tb00755.x

    CrossRef Google Scholar

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

    CrossRef Google Scholar

    [9] 龚全胜, 刘明强, 李海林, 梁明宏, 代文军. 2002. 甘肃北山造山带类型及基本特征[J]. 西北地质, 35(3): 28−34. doi: 10.3969/j.issn.1009-6248.2002.03.004

    CrossRef Google Scholar

    [10] 龚全胜, 刘明强, 梁明宏, 李海林. 2003. 北山造山带大地构造相及构造演化[J]. 西北地质, 36(1): 11−17. doi: 10.3969/j.issn.1009-6248.2003.01.002

    CrossRef Google Scholar

    [11] 何世平, 任秉琛, 姚文光, 付力浦. 2002. 甘肃内蒙古北山地区构造单元划分[J]. 西北地质, 35(4): 30−40. doi: 10.3969/j.issn.1009-6248.2002.04.004

    CrossRef Google Scholar

    [12] 何世平, 周会武, 任秉探, 姚文光, 付力浦. 2005. 甘肃内蒙古北山地区古生代地壳演化[J]. 西北地质, 38(3): 6−15. doi: 10.3969/j.issn.1009-6248.2005.03.002

    CrossRef Google Scholar

    [13] 胡新茁, 赵国春, 胡新悦, 廖云峰, 程海峰. 2015. 内蒙古北山地区月牙山蛇绿质构造混杂岩带地质特征、形成时代及大地构造意义[J]. 地质通报, 34(2–3): 425−436.

    Google Scholar

    [14] 黄增保, 金霞. 2006. 甘肃红石山地区白山组火山岩地质特征及构造背景[J]. 甘肃地质, 15(1): 19−24.

    Google Scholar

    [15] 贾元琴, 赵志雄, 许海, 王新亮, 刘强, 王金荣. 2016. 北山风雷山地区白山组流纹岩LA–ICP–MS锆石U–Pb年龄及构造环境[J]. 中国地质, 43(1): 91−98. doi: 10.3969/j.issn.1000-3657.2016.01.006

    CrossRef Google Scholar

    [16] 廖云峰, 胡新茁, 程海峰, 徐旭明. 2016. 内蒙古月牙山蛇绿岩的岩石学、地球化学特征及其地质意义[J]. 地质通报, 35(8): 1243−1254. doi: 10.3969/j.issn.1671-2552.2016.08.005

    CrossRef Google Scholar

    [17] 卢进才, 牛亚卓, 魏仙样, 陈高潮, 李玉宏. 2013. 北山红石山地区晚古生代火山岩LA–ICP–MS锆石U–Pb年龄及其构造意义[J]. 岩石学报, 29(8): 2685−2694.

    Google Scholar

    [18] 聂风军, 江思宏, 白大明. 2002. 北山地区金属矿床成矿规律及找矿方向[M]. 北京: 地质出版社, 1–408.

    Google Scholar

    [19] 聂凤军, 江思宏, 白大明, 刘妍, 张义, 赵月明, 安存杰, 王新亮, 苏新旭. 2003. 蒙甘新相邻(北山)地区金铜矿床时空分布特征及成矿作用[J]. 矿床地质, 22(3): 234−245. doi: 10.3969/j.issn.0258-7106.2003.03.003

    CrossRef Google Scholar

    [20] 牛文超, 辛后田, 段连峰, 王根厚, 赵泽霖, 张国震, 郑艺龙. 2019. 内蒙古北山地区百合山蛇绿混杂岩带的厘定及其洋盆俯冲极性—基于1∶5万清河沟幅地质图的新认识[J]. 中国地质, 46(5): 977−994. doi: 10.12029/gc20190503

    CrossRef Google Scholar

    [21] 潘志龙, 王硕, 邱振, 张欢, 张金龙, 田粉英, 李庆喆, 季虹. 2017. 内蒙古北山地区咸水沟一带早石炭世红柳园组火山岩地球化学、锆石U–Pb年龄及Hf同位素特征[J]. 地质调查与研究, 40(2): 99−108.

    Google Scholar

    [22] 任邦方, 段连峰, 李敏, 牛文超, 任云伟. 2020. 内蒙古北山哈珠地区晚古生代花岗岩类年代学与地球化学测试数据集[DB/OL]. 地质科学数据出版系统. (2020-06-30). DOI:10.35080/data.A.2020.P5.

    Google Scholar

    [23] 任云伟, 任邦方, 牛文超, 孙立新, 李敏, 张阔, 张家辉, 段连峰. 2019. 内蒙古哈珠地区石炭纪白山组火山岩: 北山北部晚古生代活动陆缘岩浆作用的产物[J]. 地球科学, 44(1): 312−327.

    Google Scholar

    [24] 孙立新, 张家辉, 任邦方, 牛文超, 任云伟, 张阔. 2017. 北山造山带白云山蛇绿混杂岩的地球化学特征、时代及地质意义[J]. 岩石矿物学杂志, 36(2): 131−147. doi: 10.3969/j.issn.1000-6524.2017.02.001

    CrossRef Google Scholar

    [25] 王国强, 李向民, 徐学义, 余吉远, 武鹏. 2014. 甘肃北山红石山蛇绿岩锆石U–Pb年代学研究及构造意义[J]. 岩石学报, 30(6): 1685−1694.

    Google Scholar

    [26] 徐学义, 何世平, 王洪亮, 陈隽璐, 张二朋, 冯益民. 2008. 中国西北部地质概论—秦岭、祁连、天山地区[M]. 北京: 科学出版社, 1–355.

    Google Scholar

    [27] 杨富林, 邹运鑫, 曹霞, 杨亮, 马刚, 高鉴. 2017. 内蒙古北山地区蓬勃山南石英闪长岩LA–ICPMS锆石U–Pb测年及其意义[J]. 地质调查与研究, 40(2): 109−118. doi: 10.3969/j.issn.1672-4135.2017.02.004

    CrossRef Google Scholar

    [28] 杨合群, 李英, 李文明, 杨建国, 赵国斌, 孙南一, 王小红, 谭文娟. 2008. 北山成矿构造背景概论[J]. 西北地质, 41(1): 22−28. doi: 10.3969/j.issn.1009-6248.2008.01.002

    CrossRef Google Scholar

    [29] 杨合群, 李英, 赵国斌, 李文渊, 王小红, 姜寒冰, 谭文娟, 孙楠一. 2010. 北山蛇绿岩特征及构造属性[J]. 西北地质, 43(1): 26−36. doi: 10.3969/j.issn.1009-6248.2010.01.002

    CrossRef Google Scholar

    [30] 尹明, 李家熙. 2011. 岩石矿物分析(第二分册)[M]. 第四版次. 北京: 地质出版社, 1–862.

    Google Scholar

    [31] 赵志雄, 贾元琴, 许海, 王金荣, 王新亮, 刘强. 2015. 北山交叉沟石英闪长岩锆石LA-ICP-MS U-Pb年龄及构造意义[J]. 地质学报, 89(7): 1210−1218. doi: 10.3969/j.issn.0001-5717.2015.07.005

    CrossRef Google Scholar

    [32] 赵志雄, 贾元琴, 王金荣, 许海, 熊煜, 王新亮, 刘强, 高伟, 高鉴, 刘孟合. 2018. 内蒙古小黑山地区二长花岗岩和石英闪长岩的锆石U–Pb年代学、元素地球化学及其地质意义[J]. 地球科学, 43(S2): 49−59.

    Google Scholar

    [33] 左国朝, 何国琦. 1990. 北山板块构造及成矿规律[M]. 北京: 北京大学出版社, 1–226.

    Google Scholar

    [34] 左国朝, 刘义科, 刘春燕. 2003. 甘新蒙北山地区构造格局及演化[J]. 甘肃地质学报, 12(1): 1−15.

    Google Scholar

    [1] Andersen T. 2002. Correction of common lead in U-Pb analyses that do not report 204Pb[J]. Chemical Geology, 192: 59−79. doi: 10.1016/S0009-2541(02)00195-X

    CrossRef Google Scholar

    [2] Geng Jianzhen, Li Huaikun, Zhang Jian, Zhou Hongying, Li Huimin. 2011. Zircon Hf isotope analysis by means of LA-MC-ICP-MS[J]. Geological Bulletin of China, 30(10): 1508−1513 (in Chinese with English abstract).

    Google Scholar

    [3] Gong Quansheng, Liu Mingqiang, Li Hailin, Liang Minghong, Dai Wenjun. 2002. The type and basic characteristics of Beishan orogenic belt, Gansu[J]. Northwestern Geology, 35(3): 28−34 (in Chinese with English abstract).

    Google Scholar

    [4] Gong Quansheng, Liu Mingqiang, Liang Minghong, Li Hailin. 2003. The tectonic facies and tectonic evolution of Beishan Orogenic Belt, Gansu[J]. Northwestern Geology, 36(1): 11−17 (in Chinese with English abstract).

    Google Scholar

    [5] He Shiping, Ren Bingshen, Yao Wenguang, Fu Lipu. 2002. The division of tectonic units of Beishan area, Gansu-Inner Mongolia[J]. Northwestern Geology, 35(4): 30−40 (in Chinese with English abstract).

    Google Scholar

    [6] He Shiping, Zhou Huiwu, Ren Bingshen, Yao Wenguang, Fu Lipu. 2005. Crustal Evolution of Palaeozoic in Beishan Area, Gansu and Inner Mongona, China[J]. Northwestern Geology, 38(3): 6−15 (in Chinese with English abstract).

    Google Scholar

    [7] Hu Xinzhuo, Zhao Guochun, Hu Xinyue, Liao Yunfeng, Cheng Haifeng. 2015. Geological characteristics, formation epoch and geotectonic significance of the Yueyashan ophiolitic tectonic Mélange in Beishan area, Inner Mongolia[J]. Geological Bulletin of China, 34(2-3): 425−436 (in Chinese with English abstract).

    Google Scholar

    [8] Huang Zenbao, Jin Xia. 2006. Geological characteristics and its setting for volcanic rocks of Baishan formation in hongshishan area of Gansu province[J]. Gansu Geology, 15(1): 19−24 (in Chinese with English abstract).

    Google Scholar

    [9] Jackson Simon E, Pearson Norman J, Griffin William L, Belousova Elena A. 2004. The application of laser ablation-inductively coupled plasma-mass spectrometry to in situ U–Pb zircon geochronology[J]. Chemical Geology, 211: 47−69. doi: 10.1016/j.chemgeo.2004.06.017

    CrossRef Google Scholar

    [10] Jia Yuanqin, Zhao Zhixiong, Xu Hai, Wang Xinliang, Liu Qiang, Wang Jinrong. 2016. Zircon LA-ICP-MS U-Pb dating of and tectonic setting of rhyolites from Baishan formation in Fengleishan area of the Beishan orogenic belt[J]. Geology in China, 43(1): 91−98 (in Chinese with English abstract).

    Google Scholar

    [11] Liao Yunfeng, Hu Xinzhuo, Cheng Haifeng, Xu Xuming. 2016. Petrological and petrochemical characteristics and geological significance of Yueyashan ophiolite[J]. Geological Bulletin of China, 35(8): 1243−1254 (in Chinese with English abstract).

    Google Scholar

    [12] Liu Yongsheng, GaoShan, Hu Zhaochu, Gao Changgui, Zong Keqing, Wang Dongbing. 2010. 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, 51(1-2): 537−571. doi: 10.1093/petrology/egp082

    CrossRef Google Scholar

    [13] Lu Jincai, Niu Yazhuo, Wei Xianyang, Chen Gaochao, Li Yuhong. 2013. LA-ICP-MS zircon U-Pb dating of the Late Paleozoic volcanic rocks from the Hongshishan area of the Beishan orogenic belt and its tectonic significances[J]. Acta Petrologica Sinica, 29(8): 2685−2694 (in Chinese with English abstract).

    Google Scholar

    [14] Ludwing KR. 2003. Isoplot/Ex Version 3.00: A Geochronological Toolkit for Microsoft Excel[J]. Berkeley Geochronology Center Special Publication, 4: 1−70.

    Google Scholar

    [15] Nie Fengjun, Jiang Sihong, Bai Daming. 2002. Metallogenic studies and ore prospecting in the conjunctin area of Inner Mongolia autonomous region, Gansu province and Xinjiang Uygur autonomous region(Beishan Mt.), Northwest China[M]. Beijing: Geological Publishing House, 1–408(in Chinese with English abstract).

    Google Scholar

    [16] Nie Fengjun, Jiang Sihong, Bai Daming, Liu Yan, Zhang Yi, Zhao Yueming, An Chunjie, Wang Xinliang, Su Xinxu. 2003. Temporal-Spatial distribution and metallogenic processes of gold and copper deposits in Inner Mongolia-Gansu-Xinjiang border(Beishan) region[J]. Mineral Deposits, 22(3): 234−245 (in Chinese with English abstract).

    Google Scholar

    [17] Niu Wenchao, Xin Houtian, Duan Lianfeng, Wang Genhou, Zhao Zelin, Zhang Guozhen, Zheng Yilong. 2019. The identification and subduction polarity of the Baiheshan ophiolite mélanges belt in the Beishan area, Inner Mongolia—New understanding based on the geological map of Qinghegou Sheet (1∶50 000)[J]. Geology in China, 46(5): 977−994 (in Chinese with English abstract).

    Google Scholar

    [18] Pan Zhilong, Wang Shuo, Qiu Zhen, Zhang Huan, Zhang Jinlong, Tian Fenying, Li Qingzhe, Ji Hong. 2017. Geochemistry, zircon U-Pb ages and Hf isotopes of the Early Carboniferous Hongliuyuan volcanic rocks in Xianshuigou, Beishan area, Inner Mongolia[J]. Geological Survey and Research, 40(2): 99−108 (in Chinese with English abstract).

    Google Scholar

    [19] Ren Bangfang, Duan Lianfeng, Li Min, Niu Wenchao, Ren Yunwei. 2020. Geochronological and Geochemical Dataset of Late Paleozoic Granitoids in the Hazhu Area of Beishan, Inner Mongolia [DB/OL]. Geoscientific Data & Discovery Publishing System. (2020-06-30). DOI: 10.35080/data.A.2020.P5.

    Google Scholar

    [20] Ren Yunwei, Ren Bangfang, Niu Wenchao, Sun Lixin, Li Min, Zhang Kuo, Zhang Jiahui, Duan Lianfeng. 2019. Carboniferous volcanics from the Baishan formation in the Hazhu area, Inner Mongolia: implications for the late Paleozoic active continental margin magmatism in the northern Beishan[J]. Earth Science, 44(1): 312−327 (in Chinese with English abstract).

    Google Scholar

    [21] Sun Lixin, Zhang Jiahui, Ren Bangfang, Niu Wenchao, Ren Yunwei, Zhang Kuo. 2017. Geochemical characteristics and U-Pb age of Baiyunshan ophiolite mélange in the Beishan orogenic belt and their geological implications[J]. Acta Petrologica et Mineralogica, 36(2): 131−147 (in Chinese with English abstract).

    Google Scholar

    [22] Wang Guoqiang, Li Xiangmin, Xu Xueyi, Yu Jiyuan, Wu Peng. 2014. Ziron U−Pb chronological study of the Hongshishan ophiolite in the Beishan area and their tectonic significance[J]. Acta Petrologica Sinica, 30(6): 1685−1694 (in Chinese with English abstract).

    Google Scholar

    [23] Whitney DL, Evans BW. 2010. Abbreviations for names of rock-forming minerals[J]. American Mineralogist, 95: 185−187. doi: 10.2138/am.2010.3371

    CrossRef Google Scholar

    [24] Xiao WJ, Mao QG, Windley BF, Han C M, Qu J F, Zhang J E, Ao S J, Guo Q Q, Cleven N R, Lin S F, Shan Y H, Li J L. 2010. Paleozoic multiple accretionary and collisional processes of the Beishan orogenic collage[J]. American Journal of Science, 310(10): 1553−1594. doi: 10.2475/10.2010.12

    CrossRef Google Scholar

    [25] Xu Xueyi, He Shiping, Wang Hongliang, Chen Junlu, Zhang Erpeng, Feng Yiming. 2008. Outline of the Geology of NW China—Qinling, Qilian and Tian Shan Areas[M]. Beijing: Science Press, 1–355(in Chinese).

    Google Scholar

    [26] Yang Fulin, Zou Yunxin, Cao Xia, Yang Liang, Ma Gang, Gao Jian. 2017. Zircon LA-ICPMS U-Pb dating for the quartz diorite in the south Pengboshan of Beishan area, Inner Mongolia[J]. Geological Survey and Research, 40(2): 109−118 (in Chinese with English abstract).

    Google Scholar

    [27] Yang Hequn, Li Ying, Li Wenming, Yang Jianguo, Zhao Guobin, Sun Nanyi, Wang Xiaohong, Tan Wenjuan. 2008. General discussion on metallogenitic tectonic setting of Beishan mountain, Northwestern China[J]. Northwestern Geology, 41(1): 22−28 (in Chinese with English abstract).

    Google Scholar

    [28] Yang Hequn, Li Ying, Zhao Guobin, Li Wenyuan, Wang Xiaohong, Jiang Hanbin, Tan Wenjuan, Sun Nanyi. 2010. Character and structural attribute of the Beishan ophiolite[J]. Northwestern Geology, 43(1): 26−36 (in Chinese with English abstract).

    Google Scholar

    [29] Yin Ming, Li Jiaxi. 2011. Rock and mineral analysis(volume Ⅱ)[M]. Fourth Edition. Beijing: Geological Publishing House, 1–862(in Chinese).

    Google Scholar

    [30] Yuan HL, Gao S, Liu XM, Li HM, Detlef G, Wu FY. 2004. Accurate U-Pb Age and Trace Element Determinations of Zircon by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry[J]. Geostandards and Geoanalytical Research, 28(3): 353−370. doi: 10.1111/j.1751-908X.2004.tb00755.x

    CrossRef Google Scholar

    [31] Zhao Zhixiong, Jia Yuanqin, Xu Hai, Wang Jinrong, Wang Xinliang, Liu Qiang. 2015. LA-ICP-MS zircon U–Pb age of quartz diorite from the Jiaochagou area in Beishan orogenic belt, Inner Mongolia, and its tectonic significance[J]. Acta Geologica Sinica, 89(7): 1210−1218 (in Chinese with English abstract).

    Google Scholar

    [32] Zhao Zhixiong, Jia Yuanqin, Wang Jinrong, Xu Hai, Xiong Yu, Wang Xinliang, Liu Qiang, Gao Wei, Gao Jian. 2018. LA-ICP-MS zircon U–Pb age of monzonite granite-quartz diorite pluton in Xiaoheishan area of Beishan orogenic belt and its geological significance, Inner Mongolia[J]. Earth Science, 43(S2): 49−59 (in Chinese with English abstract).

    Google Scholar

    [33] Zuo Guochao, He Guoqi. 1990. Plate tectonics and metallogenic regularities in Beishan region[M]. Beijing: Peking University Press, 1–226(in Chinese).

    Google Scholar

    [34] Zuo Guochao, Liu Yike, Liu Chunyan. 2003. Framework and evolution of the tectonic structure in Beishan area across Gansu province, Xinjiang autonomous region and Inner Mongolia autonomous region[J]. Acta Geologica Gansu, 12(1): 1−15 (in Chinese with English abstract).

    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(6)

Tables(8)

Export Citation
PDF
XML

Article Metrics

Article views(1000) PDF downloads(78) 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