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): 86-98
Next Article Previous Article

TENG Xuejian, CHENG Xianyu, DUAN Xiaolong, LIU Yang, TENG Fei, GUO Shuo, HE Peng, WANG Wenlong, TIAN Jian. 2020. 1∶50 000 Geological Map Database of the Juligetai Map-sheet, Inner Mongolia[J]. Geology in China, 47(S1): 86-98. doi: 10.12029/gc2020Z109
Citation: TENG Xuejian, CHENG Xianyu, DUAN Xiaolong, LIU Yang, TENG Fei, GUO Shuo, HE Peng, WANG Wenlong, TIAN Jian. 2020. 1∶50 000 Geological Map Database of the Juligetai Map-sheet, Inner Mongolia[J]. Geology in China, 47(S1): 86-98. doi: 10.12029/gc2020Z109
shu

1∶50 000 Geological Map Database of the Juligetai Map-sheet, Inner Mongolia

    Fund Project: China Geological Survey Project titled ‘Pilot Mapping of Special Geological and Geomorphological Areas’ (No.: 12120113056300)
More Information
  • Author Bio: TENG Xuejian, male, born in 1980, master, senior engineer, mainly engages in structural geology and regional geological surveying; E-mail: 451405400@qq.com
Received Date:  26 April 2020
Revised Date:  29 May 2020
Publish Date:  25 June 2020
    Abstract

  • The 1∶50 000 Geological Map of the Juligetai Map-sheet (K48E017019), Inner Mongolia was compiled according to the ‘Technical Requirements for Regional Geological Surveys (1∶50 000)’ (DD 2006-XX) and other uniform standards and requirements. It also makes full use of the data from the 1∶200 000 regional geological survey and 1∶50 000 mineral resource survey, and adopts various remote sensing imagery systems including Spot, ETM and Aster. It is an important mapping achievement guided by the orogenic belt theory. In the current project, a geological mapping method for complex tectonic areas was used to creatively express the structural features in multiple stages and their attitude features in geological maps. The map comprehensively reflects the spatial distribution of different intrusive bodies and magmatic sequence of intrusive rocks in the Wulatehou Banner in Langshan area, as well as the rhythm and deformation characteristics, sedimentary age and sedimentary environment of metamorphic sedimentary rocks of the Zhaertaishan Group. The wall-rocks of the Huogeqi Copper Deposit was further identified as carbonaceous-calcareous slates of the Agulugou Formation’s second member. The deposit is mostly located at the hinge zone of the schistose fold in the stratum. The map database includes 3 informal mapping units, 12 official mapping units, 3 periods of magmatic events and 3 tectonic deformations, in addition to 120 pieces of petrochemical analysis data and zircon U–Pb age data of 13 samples, with a data size of 106 MB. The database represents an exemplary result of the 1∶50 000 orogenic belt geological survey. It plays a leading role in orogenic belt mapping and is able to support subsequent basic geological research and prospecting by providing essential basic data.

    • FullText(HTML)
  • 加载中
    • References
  • [1] Allen M B, Windley B F, Zhang C. 1993. Palaeozoic collisional tectonics and magmatism of the Chinese Tien Shan, Central Asia[J]. Tectonophysics, 220(1–4): 89−115.

    Google Scholar

    [2] Allen M B, Engor A M C, Natalin B A. 1995. Junggar, Turfan and Alakol basins as Late Permian to Early Triassic extensional structures in a sinistral shear zone in the Altaid orogenic collage. Central Asia[J]. Journal of the Geological Society (London), 152(2): 32−338.

    Google Scholar

    [3] Coleman R G. 1989. Continental growth of Northwest China[J]. Tectonics, 8(3): 621−635. doi: 10.1029/TC008i003p00621

    CrossRef Google Scholar

    [4] Gao J, Li M S, Xiao X C, Tang Y Q, He G Q. 1998. Paleozoic tectonic evolution of the Tianshan orogen, northwestern China[J]. Tectonophysics, 287(1–4): 213−231.

    Google Scholar

    [5] Han B F, He G Q, Wang X C, Guo Z J. 2011. 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, 109: 74−93. doi: 10.1016/j.earscirev.2011.09.001

    CrossRef Google Scholar

    [6] Jahn B M, Griffin W L and Windley B F. 2000. Continental growth in the Phanerozoic: Evidence from Central Asia[J]. Tectonophysics, 328(1): vii–x.

    Google Scholar

    [7] Li Y J, Wang G H, Santosh M., Wang J F, Dong P P, Li H Y 2018. Supra-subduction zone ophiolites from Inner Mongolia, North China: Implications for the tectonic history of the southeastern Central Asian Orogenic Belt[J]. Gondwana Research, 59: 126−143. doi: 10.1016/j.gr.2018.02.018

    CrossRef Google Scholar

    [8] Li Y J, Wang G H, Santosh M, Wang J F, Dong P P, Li H Y. 2020. Subduction initiation of the SE Paleo-Asian Ocean: Evidence from a well preserved intra-oceanic forearc ophiolite fragment in central Inner Mongolia, North China[J]. Earth and Planetary Science Letters, 535: 116087. doi: 10.1016/j.jpgl.2020.116087

    CrossRef Google Scholar

    [9] Liu M, Zhang D, Xiong G Q, Zhao H T, Di Y J, Wang Z, Zhou Z G. 2016. 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, 120: 139−158. doi: 10.1016/j.jseaes.2016.01.005

    CrossRef Google Scholar

    [10] Peng R M, Zhai Y S, Li C S, Ripley E M. 2013. The Erbutu Ni-Cu deposit in the Central Asian Orogenic Belt: a Permian magmatic sulfide deposit related to Boninitic magmatism in an arc setting[J]. Economic Geology, 108: 1879−1888. doi: 10.2113/econgeo.108.8.1879

    CrossRef Google Scholar

    [11] Sengor A M C, Natalin B A, Burtman V S. 1993. Evolution of the Altaid tectonic collage and Palaeozoic crustal growth in the Eurasia[J]. Nature, 364: 299−304. doi: 10.1038/364299a0

    CrossRef Google Scholar

    [12] Wang X Y, Yuan C, Zhang Y Y, Long X P, Sun M, Wang LX, Soldner J, Lin Z F. 2018. S-type granite from the Gongpoquan arc in the Beishan Orogenic Collage, southern Altaids: Implications for the tectonic transition[J]. Journal of Asian Earth Sciences, 153: 206−222. doi: 10.1016/j.jseaes.2017.07.037

    CrossRef Google Scholar

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

    CrossRef Google Scholar

    [14] Windley B F, Allen M B, Zhang C, Zhao Z Y, Wang GR. 1990. Paleozoic accretion and Cenozoic redeformation of the Chinese Tien Shan range, Central Asia[J]. Geology, 18(2): 128−131. doi: 10.1130/0091-7613(1990)018<0128:PAACRO>2.3.CO;2

    CrossRef Google Scholar

    [15] Windley B F, Alexeiev D, Xiao W J, Kröner A. 2007. Badarch G.Tectonics models for accretion of the Central Asian Orogenic Belt[J]. Journal of the Geological Society, 164: 31−47. doi: 10.1144/0016-76492006-022

    CrossRef Google Scholar

    [16] Wu T R, He G Q, Zhang C. 1998. On Paleozoic tectonics in the Alxa region, Inner Mongolia, China[J]. Acta Geologica Sinica(English Edition), 72(3): 256−263.

    Google Scholar

    [17] Xiao W J, Windley B F, Badarch G, Sun S, Li J L, Qin K Z, Wang Z H. 2004. Palaeozoic accretionary and convergent tectonics of the southern Altaids: Implications for the growth of Central Asia[J]. Journal of the Geological Society, 161(3): 339−342. doi: 10.1144/0016-764903-165

    CrossRef Google Scholar

    [18] Xiao W J, Mao Q G, Windley B F, 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: 1553−1594. doi: 10.2475/10.2010.12

    CrossRef Google Scholar

    [19] Xu B, Charvet J, Chen Y, Zhao P, Shi G Z. 2013. 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, 23: 1342−1364. doi: 10.1016/j.gr.2012.05.015

    CrossRef Google Scholar

    [20] Xu Z, Han B F, Ren R, Zhou Y Z, Zhang L, Chen J F, Su L, Li X H, Liu D Y. 2012. Ultramafic-mafic mélange, island arc and post-collisional intrusions in the Mayile Mountain, West Junggar, China: implications for Paleozoic intraoceanic subduction-accretion process[J]. Lithos, 132–133: 141−161.

    Google Scholar

    [21] Yuan Y, Zong K Q, He Z Y, Klemd R, Jiang H Y, Zhang W, Liu Y S, Hu Z C, Zhang Z M. 2018. Geochemical evidence for Paleozoic crustal growth and tectonic conversion in the Northern Beishan Orogenic Belt, southern Central Asian Orogenic Belt[J]. Lithos, 302–303: 189−202.

    Google Scholar

    [22] Zhang W, Jian P, Kröner A, S hi, Y R. 2013. Magmatic and metamorphic development of an early to mid-Paleozoic continental margin arc in the southernmost Central Asian Orogenic Belt, Inner Mongolia, China[J]. Journal of Asian Earth Sciences, 72: 63−74. doi: 10.1016/j.jseaes.2012.05.025

    CrossRef Google Scholar

    [23] Zhang X H, Gao Y L, Wang Z J, Liu H, Ma Y G. 2012. Carboniferous appinitic intrusions from the northern North China craton: geochemistry, petrogenesis and tectonic implications[J]. Journal of the Geological Society, 169(3): 337−351. doi: 10.1144/0016-76492011-062

    CrossRef Google Scholar

    [24] Zheng R G, Xiao W J, Li J Y, Wu T R, Zhang W. 2018. A Silurian-early Devonian slab window in the southern Central Asian Orogenic Belt: Evidence from high-Mg diorites, adakites and granitoids in the western Central Beishan region, NW China[J]. Journal of Asian Earth Sciences, 153: 75−99. doi: 10.1016/j.jseaes.2016.12.008

    CrossRef Google Scholar

    [25] 白瑾. 2003. 造山带构造样式的恢复及其构造环境意义[J]. 地质调查与研究, 6(1): 38−44. doi: 10.3969/j.issn.1672-4135.2003.01.007

    CrossRef Google Scholar

    [26] 冯丽霞, 张志诚, 韩宝福, 任荣, 李建锋, 苏犁. 2013. 内蒙古达茂旗花岗岩类 LA–ICP–MS 锆石 U–Pb 年龄及其地质意义[J]. 地质通报, 32(11): 1737−1748. doi: 10.3969/j.issn.1671-2552.2013.11.006

    CrossRef Google Scholar

    [27] 刘烨. 2012. 内蒙古东升庙地区花岗片麻岩和侵入岩的地球化学、年代学特征及构造意义[D].兰州: 兰州大学博士学位论文.

    Google Scholar

    [28] 刘洋, 郭硕, 滕学建, 滕飞. 2020. 内蒙古居力格台幅 1∶50 000 地质图数据库[DB/OL]. 地质科学数据出版系统. (2020-06-30). DOI: 10.35080/data.A.2020.P9.

    Google Scholar

    [29] 毛晓长. 2018. 2018年全国区域地质调查优秀图幅展评会召开[J]. 中国地质, 45(S2): 93. doi: 10.12029/gc2018S211

    CrossRef Google Scholar

    [30] 内蒙古自治区第一区域地质调查队. 1982. 1∶20万区域地质矿产调查报告(三道桥幅)[R].

    Google Scholar

    [31] 滕学建, 田健, 刘洋, 张永, 滕飞, 段霄龙. 2019. 内蒙古狼山地区早志留世石英闪长岩体的厘定及其地质意义[J]. 地球科学, 44(4): 1236−1247.

    Google Scholar

    [32] 田健, 滕学建, 刘洋, 滕飞, 何鹏, 郭硕, 王文龙. 2018. 内蒙古狼山地区早石炭世角闪辉长岩、花岗闪长岩的岩石成因及构造意义[J]. 岩石矿物学杂志, 37(5): 60−76.

    Google Scholar

    [33] 王树庆, 胡晓佳, 赵华雷. 2019. 内蒙古苏左旗洪格尔地区新发现晚石炭世碱性花岗岩[J]. 地质调查与研究, 42(2): 81−85. doi: 10.3969/j.issn.1672-4135.2019.02.001

    CrossRef Google Scholar

    [34] 吴飞, 张拴宏, 赵越, 叶浩. 2014. 华北地块北缘内蒙古固阳地区早二叠世岩体的侵位深度及其构造意义[J]. 中国地质, 41(3): 824−837. doi: 10.3969/j.issn.1000-3657.2014.03.011

    CrossRef Google Scholar

    [35] 张维, 简平. 2012. 华北北缘固阳二叠纪闪长岩-石英闪长岩-英云闪长岩套 HSRIMP 年代学[J]. 中国地质, 39(6): 1593−1603. doi: 10.3969/j.issn.1000-3657.2012.06.009

    CrossRef Google Scholar

    [36] 赵闯, 苏旭亮, 薛斌, 程东江, 史兴俊, 宋涛涛, 张阔. 2020. 内蒙古西部苦楚乌拉-英巴地区花岗岩锆石U–Pb定年及地球化学特征[J/OL]. 中国地质, 1–22 [2020-06-02].

    Google Scholar

    [37] 赵磊, 牛宝贵, 徐芹芹, 杨亚琦. 2019. 新疆东准噶尔卡拉麦里蛇绿岩带两侧志留—石炭系沉积和构造特征分析及其意义[J]. 中国地质, 46(3): 615−628. doi: 10.12029/gc20190312

    CrossRef Google Scholar

    [1] Allen MB, Windley BF, Zhang C. 1993. Palaeozoic collisional tectonics and magmatism of the Chinese Tien Shan, Central Asia[J]. Tectonophysics, 220(1–4): 89−115.

    Google Scholar

    [2] Allen MB, Engor AMC, Natalin BA. 1995. Junggar, Turfan and Alakol basins as Late Permian to Early Triassic extensional structures in a sinistral shear zone in the Altaid orogenic collage. Central Asia[J]. Journal of the Geological Society (London), 152(2): 32−338.

    Google Scholar

    [3] Bai Jin. 2003. Recovery of structural styles of orogenic belt and its tectonic environmental significance[J]. Geological survey and research, 6(1): 38−44, 51 (in Chinese with English abstract).

    Google Scholar

    [4] Coleman RG. 1989. Continental growth of Northwest China[J]. Tectonics, 8(3): 621−635. doi: 10.1029/TC008i003p00621

    CrossRef Google Scholar

    [5] Feng Lixia, Zhang Zhicheng, Han Baofu, Ren Rong, Li Jianfeng, Su Li. 2013. LA-ICP-MS zircon U–Pb ages of granitoids in Darhan Muminggan Joint Banner, Inner Mongolia, and their geological significance[J]. Geological Bulletin of China, 32(11): 1737−1748 (in Chinese with English abstract).

    Google Scholar

    [6] Gao J, Li MS, Xiao XC, Tang YQ, He GQ. 1998. Paleozoic tectonic evolution of the Tianshan orogen, northwestern China[J]. Tectonophysics, 287(1–4): 213−231.

    Google Scholar

    [7] Han BF, He GQ, Wang XC, Guo ZJ. 2011. 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, 109: 74−93. doi: 10.1016/j.earscirev.2011.09.001

    CrossRef Google Scholar

    [8] Jahn BM, Griffin WL, Windley BF. 2000. Continental growth in the Phanerozoic: Evidence from Central Asia[J]. Tectonophysics, 328(1): vii−x.

    Google Scholar

    [9] Li YJ, Wang GH, Santosh M., Wang JF, Dong PP, Li HY 2018. Supra-subduction zone ophiolites from Inner Mongolia, North China: Implications for the tectonic history of the southeastern Central Asian Orogenic Belt[J]. Gondwana Research, 59: 126−143. doi: 10.1016/j.gr.2018.02.018

    CrossRef Google Scholar

    [10] Li YJ, Wang GH, Santosh M, Wang JF, Dong PP, Li HY. 2020. Subduction initiation of the SE Paleo-Asian Ocean: Evidence from a well preserved intra-oceanic forearc ophiolite fragment in central Inner Mongolia, North China[J]. Earth and Planetary Science Letters, 535: 116087. doi: 10.1016/j.jpgl.2020.116087

    CrossRef Google Scholar

    [11] Liu M, Zhang D, Xiong GQ, Zhao HT, Di YJ, Wang Z, Zhou ZG. 2016. 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, 120: 139−158. doi: 10.1016/j.jseaes.2016.01.005

    CrossRef Google Scholar

    [12] Liu Ye. 2012. Geochemical and Chronological Characteristics of the Granitic Gneisses and Intrusive Rocks from Dongshengmiao Region, Inner Mongolia and Their Tectonic Implications[D]. Lanzhou: Doctoral dissertation of Lanzhou University (in Chinese with English abstract).

    Google Scholar

    [13] Liu Yang, GuoShuo, Teng Xuejian, Teng Fei. 2020. 1∶50 000 Geological Map Database of the Juligetai Map-sheet, Inner Mongolia[DB/OL]. Geoscientific Data & Discovery Publishing System. (2020-06-30). DOI: 10.35080/data.A.2020.P9.

    Google Scholar

    [14] Mao Xiaochang. 2018. 2018 National exhibition and evaluation conference on excellent maps of regional geological survey[J]. Geology in China, 45(S2): 119−120 (in Chinese with English abstract).

    Google Scholar

    [15] Peng RM, Zhai YS, Li CS, Ripley EM. 2013. The Erbutu Ni–Cu deposit in the Central Asian Orogenic Belt: a Permian magmatic sulfide deposit related to Boninitic magmatism in an arc setting[J]. Economic Geology, 108: 1879−1888. doi: 10.2113/econgeo.108.8.1879

    CrossRef Google Scholar

    [16] Sengor AMC, Natalin BA, Burtman VS. 1993. Evolution of the Altaid tectonic collage and Palaeozoic crustal growth in the Eurasia[J]. Nature, 364: 299−304. doi: 10.1038/364299a0

    CrossRef Google Scholar

    [17] Teng Xuejian, Tian Jian, Liu Yang, Zhang Yong, Teng Fei, Duan Xiaolong. 2019. Definition and Geological Significance of Early Silurian Quartz Diorite Pluton in Langshan area, Inner Mongolia[J]. Earth Science, 44(4): 1236−1247 (in Chinese with English abstract).

    Google Scholar

    [18] The first regional geological survey team of Inner Mongolia. 1982. 1∶200 000 regional geological and mineral survey report (Sandaoqiao Map Sheet)[R]. Inner Mongolia Autonomous Region(in Chinese).

    Google Scholar

    [19] Tian Jian, Teng Xuejian, Liu Yang, Teng Fei, Guo Shuo, He Peng, Wang Wenlong. Duan Xiaolong 2018. Petrogenesis and tectonic significance of the Early Carboniferous hornblendegabbro and granodiorite in Langshan area, Inner Mongolia[J]. Acta Petrologica Et Mineralogica, 37(5): 754−770 (in Chinese with English abstract).

    Google Scholar

    [20] Wang Shuqing, Hu Xiaojia, Zhao Hualei. 2019. New discovery of Late Carboniferous alkaline granite in the Honggeer area, Sonid Zuoqi, Inner Mongolia[J]. Geological survey and research, 42(2): 81−85 (in Chinese with English abstract).

    Google Scholar

    [21] Wang XY, Yuan C, Zhang YY, Long XP, Sun M, Wang LX, Soldner J, Lin Z F. 2018. S-type granite from the Gongpoquan arc in the Beishan Orogenic Collage, southern Altaids: Implications for the tectonic transition[J]. Journal of Asian Earth Sciences, 153: 206−222. doi: 10.1016/j.jseaes.2017.07.037

    CrossRef Google Scholar

    [22] Wang ZZ, Han BF, Feng LX, Liu B. 2015. Geochronology, geochemistry and origins of the Paleozoic–Triassic plutons in the Langshan area, western Inner Mongolia, China[J]. Journal of Asian Earth Sciences, 97: 337−351. doi: 10.1016/j.jseaes.2014.08.005

    CrossRef Google Scholar

    [23] Windley BF, Allen MB, Zhang C, Zhao ZY, Wang GR. 1990. Paleozoic accretion and Cenozoic redeformation of the Chinese Tien Shan range, Central Asia[J]. Geology, 18(2): 128−131. doi: 10.1130/0091-7613(1990)018<0128:PAACRO>2.3.CO;2

    CrossRef Google Scholar

    [24] Windley BF, Alexeiev D, Xiao WJ, Kröner A. 2007. Badarch G.Tectonics models for accretion of the Central Asian Orogenic Belt[J]. Journal of the Geological Society, 164: 31−47. doi: 10.1144/0016-76492006-022

    CrossRef Google Scholar

    [25] Wu Fei, Zhang Shuanghong, Zhao Yue, Ye Hao. 2014. Emplacement depth and tectonic significance of Early Permian pluton in Inner Mongolia Guyang area, northern margin of North China block[J]. Geology in China, 41(3): 824−837 (in Chinese with English abstract).

    Google Scholar

    [26] Wu TR, He GQ, Zhang C. 1998. On Paleozoic tectonics in the Alxa region, Inner Mongolia, China[J]. Acta Geologica Sinica, 72(3): 256−263.

    Google Scholar

    [27] Xiao WJ, Windley BF, Badarch G, Sun S, Li JL, Qin KZ, Wang ZH. 2004. Palaeozoic accretionary and convergent tectonics of the southern Altaids: Implications for the growth of Central Asia[J]. Journal of the Geological Society, 161(3): 339−342. doi: 10.1144/0016-764903-165

    CrossRef Google Scholar

    [28] Xiao W J, Mao Q G, Windley B F, 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: 1553−1594. doi: 10.2475/10.2010.12

    CrossRef Google Scholar

    [29] Xu B, Charvet J, Chen Y, Zhao P, Shi GZ. 2013. 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, 23: 1342−1364. doi: 10.1016/j.gr.2012.05.015

    CrossRef Google Scholar

    [30] Xu Z, Han BF, Ren R, Zhou YZ, Zhang L, Chen JF, Su L, Li XH, Liu DY. 2012. Ultramafic-mafic mélange, island arc and post-collisional intrusions in the Mayile Mountain, West Junggar, China: implications for Paleozoic intraoceanic subduction-accretion process[J]. Lithos, 132–133: 141−161.

    Google Scholar

    [31] Yuan Y, Zong K Q, He ZY, Klemd R, Jiang HY, Zhang W, Liu YS, Hu ZC, Zhang ZM. 2018. Geochemical evidence for Paleozoic crustal growth and tectonic conversion in the Northern Beishan Orogenic Belt, southern Central Asian Orogenic Belt[J]. Lithos, 302–303: 189−202.

    Google Scholar

    [32] Zhang Wei, Jian Ping. 2012. SHRIMP dating of the Permian Guyang diorite-granodiorite-tonalite suite in the northern margin of the North China Craton[J]. Geology in China, 39(6): 1593−1603 (in Chinese with English abstract).

    Google Scholar

    [33] Zhang W, Jian P, Kröner A, Shi YR. 2013. Magmatic and metamorphic development of an early to mid-Paleozoic continental margin arc in the southernmost Central Asian Orogenic Belt, Inner Mongolia, China[J]. Journal of Asian Earth Sciences, 72: 63−74. doi: 10.1016/j.jseaes.2012.05.025

    CrossRef Google Scholar

    [34] Zhang XH, Gao YL, Wang ZJ, Liu H, Ma YG. 2012. Carboniferous appinitic intrusions from the northern North China craton: geochemistry, petrogenesis and tectonic implications[J]. Journal of the Geological Society, 169(3): 337−351. doi: 10.1144/0016-76492011-062

    CrossRef Google Scholar

    [35] Zhao Chuang, Su Xuliang, Xue bin, Cheng Dongjiang, Shi Xingjun, song Taotao, Zhang Kuo. 2020. Zircon U-Pb dating and geochemical characteristics of granites in the area of Wula-Yingba, Kuchu, western Inner Mongolia[J/OL]. Geology in China,1–22[2020-06-02] (in Chinese with English abstract).

    Google Scholar

    [36] Zhao Lei, Niu Baogui, Xu Qinqin, Yang Yaqi. 2019. An analysis of Silurian- Carboniferous sedimentary and structural characteristics on both sides of Karamaili ophiolitic belt of Xinjiang and its significance[J]. Geology in China, 46(3): 615−628 (in Chinese with English abstract).

    Google Scholar

    [37] Zheng RG, Xiao WJ, Li JY, Wu TR, Zhang W. 2018. A Silurian-early Devonian slab window in the southern Central Asian Orogenic Belt: Evidence from high-Mg diorites, adakites and granitoids in the western Central Beishan region, NW China[J]. Journal of Asian Earth Sciences, 153: 75−99. doi: 10.1016/j.jseaes.2016.12.008

    CrossRef 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(10)

Export Citation
PDF
XML

Article Metrics

Article views(3415) PDF downloads(85) 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