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CHAO Hongli, REN Jiande, LYU Jigen, XIE Chaoyong, LI Yingqi, LI Ruiqiang, JIAO Jinghua. 2020. 1∶50 000 Geological Map Database of Sanchuan Map-sheet, Henan Province[J]. Geology in China, 47(S1): 173-188. doi: 10.12029/gc2020Z116
Citation: CHAO Hongli, REN Jiande, LYU Jigen, XIE Chaoyong, LI Yingqi, LI Ruiqiang, JIAO Jinghua. 2020. 1∶50 000 Geological Map Database of Sanchuan Map-sheet, Henan Province[J]. Geology in China, 47(S1): 173-188. doi: 10.12029/gc2020Z116
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1∶50 000 Geological Map Database of Sanchuan Map-sheet, Henan Province

    Fund Project: jointly funded by the projects titled “Geological and Mineral Survey of Zhongtiao—Xiong’ershan Metallogenic Area” (No.: DD20160043) and “1∶50 000-scale Regional Geological and Mineral Survey of Baitujie and Sanchuan Map-sheets, Henan Province” (No.: DD20160043-02) initiated by the China Geological Survey
More Information
  • Author Bio: CHAO Hongli, female, born in 1970, engineer, engages in regional geological and mineral survey; E-mail: 623337069@qq.com
  • Corresponding author: REN Jiande, male, born in 1965, professorate senior engineer, engages in regional geological survey and research, E-mail: 571950946@qq.com  
Received Date:  15 April 2020
Revised Date:  14 June 2020
Publish Date:  25 June 2020
    Abstract

  • The 1∶50 000 Geologic Map Database of Sanchuan Map-sheet (I49E013014), Henan Province (also referred to as the Database) was established using data obtained through practical measurement and digital mapping. The structural and lithologic mapping was conducted during field data acquisition, focusing on the presentation of special geological blocks and informal mapping units. The samples collected in the field included 66 samples for microscopic petrography identification, 180 samples for whole-rock petrochemical analysis, 19 samples for isotopic dating, and 21 samples for chemical analysis in total. In this study, the main achievements obtained in this map-sheet are as follows. The Taowan Group was found to have occurred during the Ordovician according to multiple taxonomic classifications and short age ranges found in its stratotype section. Alkaline volcanic intercalations were found in the Taowan Group, indicating that an extensional basin developed on the southern margin of the North China Plate in the Ordovician. The greenschists in the Sichakou Formation and Xiewan Formation of the Kuanping Group were determined to be intraplate volcanic rocks, indicating that the main part of the Kuanping Group was formed in an extensional basin. The dike swarms of Silurian alkali-feldspar granite porphyry were found in the southern part of the map-sheet by mapping, restricting the closure era of the Qinling Ocean to a time not later than the Silurian. The intrusions of the late Mesozoic were divided into five intrusive stages. The Luanchuan fault zone was determined to have undergone three stages of activities in the early Paleozoic, early Mesozoic, and late Mesozoic. Furthermore, Sinian glacial sediments were newly discovered in the map-sheet. The Database consists of data on feature classes, complex classes, and object classes, with a data size of about 63.5 MB. It fully reflects the geological and mineral achievements of the map-sheet, and will provide basic data for mineral exploration and exploitation and prevention and control of geological hazards in the map-sheet, research on the Qinling Orogenic Belt, and the popularization of geoscience.

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  • [1] Combaz A, Penignel G. 1972. Etude Palynostratigraphique de l’Ordivicien dans quelgues sondages du Bassin de Canning (Australie Occcidentale)[J]. Bull Center Rech. Pau-SNPA, 6(1): 121−167.

    Google Scholar

    [2] Dong Yunpeng, Zhao Yang, Liu Xiaoming, Zhang Xiaoning, He Dengfeng, Li Wei, Zhang Feifei, Sun Shengsi, Zhang Hongfu, Zhang Guowei. 2014. Neoproterozoic amalgamation of the Northern Qinling terrain to the North China Craton: Constraints from geochronology and geochemistry of the Kuanping ophiolite[J]. Precambrian Research, 255: 77−95. doi: 10.1016/j.precamres.2014.09.008

    CrossRef Google Scholar

    [3] Eisenack F. 1962. Mikrofossilien aus dem Ordovizium des Baltikums[J]. Senckenbergiana Lethaca, 43(5): 349−366.

    Google Scholar

    [4] Timofeev BV. 1973. Proterozoic and Early Palaeozoic microfossils[C]. Proceedings of the Third International Palynological Conference, Nauk, Moscow. 7–12.

    Google Scholar

    [5] Johnson N G. 1985. Early Silurian Palynomorphs from the Tuscarora Fromation in central Pennsylvania and their paleobotanical and geological significance[J]. Review of Palaeobotany and Palynology[J]. Palynology, 45(3–4): 307–359.

    Google Scholar

    [6] Yang Y, Chen YJ, Zhang J, Zhang C. 2013. Ore geology, fluid inclusions and four–stage hydrothermal mineralization of the Shangfanggou giant Mo–Fe deposit in Eastern Qinling, central China[J]. Ore Geology Reviews, 55: 146−161. doi: 10.1016/j.oregeorev.2013.05.007

    CrossRef Google Scholar

    [7] Yang Y, Liu ZJ, Deng XH. 2017. Mineralization mechanisms in the Shangfanggou giant porphyry-skarn Mo-Fe deposit of the east Qinling, China: Constraints from H–O–C–S–Pb isotopes[J]. Ore Geology Reviews, 81: 535−547. doi: 10.1016/j.oregeorev.2016.06.026

    CrossRef Google Scholar

    [8] 地质部物探局902队. 1960. 豫西地区1∶100 000航磁测量和航空放射性测量成果报告[R]. 德阳.

    Google Scholar

    [9] 地质部物探局903队. 1966. 豫西地区1∶50 000航磁测量成果报告[R]. 德阳.

    Google Scholar

    [10] 第五春荣, 孙勇, 刘良, 张成立, 王洪亮. 2010. 北秦岭宽坪岩群的解体及新元古代N-MORB[J]. 岩石学报, 26(7): 2015−2038.

    Google Scholar

    [11] 国家地质总局第二物探大队. 1975. 河南省栾川县三川-合峪地区水系沉积物测量研究报告[R]. 德阳.

    Google Scholar

    [12] 高联达. 1986. 云南武定、录劝早奥陶世组几丁虫[C]//中国地质科学院地层和古生物编辑委员会编辑. 地层古生物论文集. 北京: 地质出版社, 133–152.

    Google Scholar

    [13] 高联达. 1991. 云南武定下奥陶统红石岩组疑源类[J]. 地质论评, 7(5): 44−55.

    Google Scholar

    [14] 河南省地质局秦岭地质队. 1958. 1∶20万栾川幅(I49-XXII)地质报告[R]. 郑州.

    Google Scholar

    [15] 河南省地质矿产厅区域地质调查队. 1995. 河南省1∶50 000横涧幅、朱阳关幅区域地质调查报告[R]. 平顶山.

    Google Scholar

    [16] 河南省地质矿产厅. 1997. 河南省岩石地层[M]. 武汉: 中国地质大学出版社, 1–299.

    Google Scholar

    [17] 河南省地质调查院. 2002. 1∶250 000内乡县幅区域地质调查报告[R]. 郑州.

    Google Scholar

    [18] 河南省地质调查院. 2009. 河南卢氏地区矿产远景调查[R]. 郑州.

    Google Scholar

    [19] 河南省地质调查院. 2013. 河南省成矿地质背景研究成果报告[R]. 郑州.

    Google Scholar

    [20] 河南省地质三队. 1977. 1∶50 000栾川县南部区域地质调查报告[R]. 洛阳.

    Google Scholar

    [21] 河南省地质局地调一队. 1980. 河南省栾川县三道庄矿区钼钨矿详细勘探地质报告[R]. 洛阳.

    Google Scholar

    [22] 河南省物探队. 2000. 豫西南地区1∶200 000区域重力调查报告[R]. 郑州.

    Google Scholar

    [23] 霍立新, 宋传中. 2008. 栾川断裂带的构造变形与模拟[J]. 合肥工业大学学报, 31(11): 1731−1735.

    Google Scholar

    [24] 胡元绪. 1986. 陕西紫阳高桥地区早奥陶世微体古生物群及其地层意义[J]. 中国地质科学院西安地质矿产研究所(所刊), 14: 199−233.

    Google Scholar

    [25] 贾承造, 施央申, 郭令智. 1988. 东秦岭板块构造[M]. 南京: 南京大学出版社, 1–130.

    Google Scholar

    [26] 李承东, 赵利刚, 许雅雯, 常青松, 王世炎, 许腾. 2018. 北秦岭宽坪岩群变质沉积岩年代学及地质意义[J]. 中国地质, 45(5): 992−1010. doi: 10.12029/gc20180508

    CrossRef Google Scholar

    [27] 罗铭玖, 张辅民, 董群英, 许永仁, 黎世美, 李昆华. 1991. 中国钼矿床[M]. 郑州: 河南科学技术出版社, 329–351.

    Google Scholar

    [28] 卢礼昌. 1987. 湖北宜昌黄花场大湾组(Arenigian)疑源类[J]. 微体古生物学报, 4: 87−102.

    Google Scholar

    [29] 陆松年, 李怀坤, 陈志宏, 郝国杰, 周红英, 郭进京, 牛广华, 相振群. 2003. 秦岭中新元古代地质演化及对Rodinia超级大陆事件的响应[M]. 北京: 地质出版社, 120–131.

    Google Scholar

    [30] 陆松年, 于海峰, 李怀坤. 2009. 中央造山带(中西部)前寒武纪地质[M]. 北京: 地质出版社, 165–168.

    Google Scholar

    [31] 毛景文, 谢桂青, 袁顺达, 刘鹏, 孟旭阳, 周振华, 郑伟. 2018. 环太平洋成矿带斑岩-矽卡岩型铜矿和与花岗岩有关的锡多金属矿研究现状与展望[J]. 岩石学报, 34(9): 611−618.

    Google Scholar

    [32] 任建德, 吕际根, 张毅星, 晁红丽, 谢朝永, 李春艳, 李莹琪, 贺承广, 王小娟, 李瑞强, 翟文建, 焦静华, 孙学静, 李敏, 刘姗姗. 2020. 河南省三川幅 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.P16.

    Google Scholar

    [33] 陕西省地质矿产局. 1989. 陕西省区域地质志[M]. 北京: 地质出版社, 1–698.

    Google Scholar

    [34] 盛中烈, 罗铭久, 李良骏. 1980. 豫西一斑岩钼矿带的基本地质特征及主要成矿控制因素[J]. 地质学报, 4(4): 300−309.

    Google Scholar

    [35] 石铨曾, 陶自强, 庞继群, 曲明绪. 1996. 华北板块南缘栾川群研究[J]. 华北地质矿产杂志, 11(1): 52−59.

    Google Scholar

    [36] 宋传中, 张国为. 1999. 伏牛山推覆构造及其动力学控制[J]. 地质论评, 45(5): 492−497. doi: 10.3321/j.issn:0371-5736.1999.05.007

    CrossRef Google Scholar

    [37] 宋传中, 任升莲, 李加好, 陈泽超, 连芸, 蔡志川. 2009. 华北板块南缘的变形分解: 洛南-栾川断裂带与秦岭北缘强变形带研究[J]. 地学前缘, 16(3): 181−189. doi: 10.3321/j.issn:1005-2321.2009.03.014

    CrossRef Google Scholar

    [38] 王赛, 叶会寿, 杨永强, 张兴康, 苏慧敏, 杨晨英. 2016. 豫西火神庙岩体锆石U-Pb年代学、地球化学及Hf同位素组成[J]. 地球科学, 41(2): 293−316.

    Google Scholar

    [39] 王宗起, 高联达, 王涛, 姜春发. 2007. 北秦岭陶湾群发现的微体化石及其对地层时代的限定[J]. 中国科学D辑, 37(11): 1467−1473.

    Google Scholar

    [40] 王宗起, 闫全人, 闫臻, 王涛, 姜春发, 高联达. 2009. 秦岭造山带主要大地构造单元的新划分[J]. 地质学报, 83(11): 1527−1546. doi: 10.3321/j.issn:0001-5717.2009.11.001

    CrossRef Google Scholar

    [41] 阎国翰, 蔡剑辉, 任康绪, 何国琦, 牟保磊, 许保良, 李凤棠, 杨斌. 2007. 华北克拉通板内拉张性岩浆作用与三个超大陆裂解及深部地球动力学[J]. 高校地质学报, 13(2): 161−174. doi: 10.3969/j.issn.1006-7493.2007.02.003

    CrossRef Google Scholar

    [42] 闫全人, 王宗启, 闫臻, 王涛, 陈隽路, 向忠金, 张宗清, 姜春发. 2008. 秦岭造山带宽坪群的变镁铁质岩的成因、时代及其构造意义[J]. 地质通报, 27(9): 1475−1492. doi: 10.3969/j.issn.1671-2552.2008.09.010

    CrossRef Google Scholar

    [43] 叶会寿, 毛景文, 李永峰, 燕长海, 郭保健, 赵财胜, 何春芬, 郑榕芬, 陈莉. 2006. 豫西南泥湖矿田钼钨及铅锌银矿床地质特征及成矿机理探讨[J]. 现代地质, 20(1): 165−174. doi: 10.3969/j.issn.1000-8527.2006.01.019

    CrossRef Google Scholar

    [44] 中国地质调查局天津地质调查中心. 2015. 豫西关键地区区域地质调查成果报告[R]. 天津.

    Google Scholar

    [45] 中国地质调查局天津地质调查中心. 2019. 中条—熊耳山成矿区关键地区地质调查与成果集成成果报告[R]. 天津.

    Google Scholar

    [46] 张国伟, 袁学诚, 张本仁, 袁学成, 肖庆辉. 2001. 秦岭造山带与大陆动力学[M]. 北京: 科学出版社, 1–885.

    Google Scholar

    [47] 张恒, 高林志, 周洪瑞, 宋彪, 丁孝忠, 张传恒, 刘昊岗, 龚成强. 2019. 华北克拉通南缘官道口群和洛峪群的年代学研究新进展——来自凝灰岩SHRIMP锆石U-Pb年龄的新证据[J]. 岩石学报, 35(8): 2470−2486. doi: 10.18654/1000-0569/2019.08.10

    CrossRef Google Scholar

    [48] 张寿广, 万渝生, 刘国惠, 从曰祥, 赵子然. 1991. 北秦岭宽坪群变质地质[M]. 北京: 北京科学技术出版社, 1–223.

    Google Scholar

    [49] 张宗清, 张旗. 1995. 北秦岭晚元古代宽坪蛇绿岩中变质基性火山岩的地球化学特征[J]. 岩石学报, 11(增刊): 165−177.

    Google Scholar

    [1] 1st Geological Survey Team of Henan Bureau of Geo-exploration & Mineral Development. 1980.Detailed exploration geological report of molybdenum-tungsten deposits in Sandaozhuang mining area, Luanchuan County, Henan Province[R]. Luoyang (in Chinese).

    Google Scholar

    [2] 2nd Geophysical Exploration Team of the National Geological General Administration. 1975. Survey and research report of stream sediments in Sanchuan-Heyu area, Luanchuan County, Henan Province[R]. Deyang (in Chinese).

    Google Scholar

    [3] 3rd Geological Survey Team of Henan Bureau of Geo-exploration & Mineral Development. 1977. 1∶50 000 regional geological survey report of South Luanchuan County[R]. Luoyang (in Chinese).

    Google Scholar

    [4] 902nd Team of Geophysical Exploration Bureau under the Ministry of Geology and Mineral Resources. 1960. Result report of 1: 100 000-scale aeromagnetic survey and airborne radioactivity measurement in West Henan Province [R]. Deyang (in Chinese).

    Google Scholar

    [5] 903rd Team of Geophysical Exploration Bureau under the Ministry of Geology and Mineral Resources. 1966. Survey and research report of 1∶50 000-scale aeromagnetic survey in West Henan Province[R]. Deyang (in Chinese).

    Google Scholar

    [6] Combaz A, Penignel G. 1972. Etude Palynostratigraphique de l’Ordivicien dans quelgues sondages du Bassin de Canning (Australie O cccidentale)[J]. Bull Center Rech. Pau-SNPA, 6(1): 121−167.

    Google Scholar

    [7] Department of Geology and Mineral Resources of Henan Province. 1997. Rock strata of Henan Province[M]. Wuhan: China University of Geosciences Press, 1–299 (in Chinese).

    Google Scholar

    [8] Diwu CR, Sun Y, Liu L, Zhang CL, Wang HL. 2010. The disintegration of Kuanping Group in North Qinling orogenic belts and Neo-proterozoic N-MORB[J]. Acta Petrologica Sinica, 26(7): 2015−2038 (in Chinese with English abstract).

    Google Scholar

    [9] Dong YP, Zhao Y, Liu XM, Zhang XN, He DF, Li W, Zhang FF, Sun SS, Zhang HF, Zhang GW. 2014. Neoproterozoic amalgamation of the Northern Qinling terrain to the North China Craton: Constraints from geochronology and geochemistry of the Kuanping ophiolite[J]. Precambrian Research, 255: 77−95. doi: 10.1016/j.precamres.2014.09.008

    CrossRef Google Scholar

    [10] Eisennack F. 1962. Mikrofossilien aus dem Ordovizium des Baltikums[J]. Senckenbergiana Lethaca, 43(5): 349−366.

    Google Scholar

    [11] Gao LD. 1986. Chitin worms of the Early Ordovician formation in Wuding and Luquan yunnan[C]. Editorial Committee of Stratigraphy and Paleontology, Chinese Academy of Geological Sciences, Proceedings of stratigraphic Paleontology. Beijing: Geological Publishing House, 133–152 (in Chinese).

    Google Scholar

    [12] Gao LD. 1991. Wuxi-ordovician Hongshi Formation in Yunnan[J]. Geological Review, 7(5): 44−55 (in Chinese with English abstract).

    Google Scholar

    [13] Geophysical Exploration Team of Henan Bureau of Geo-exploration & Mineral Development. 2000. 1∶200 000-scale regional gravity survey report of Southwest Henan Province[R]. Zhengzhou (in Chinese).

    Google Scholar

    [14] Henan Institute of Geological Survey. 2002. 1∶250 000 scale regional geological survey report of Neixiang map-sheet[R]. Zhengzhou (in Chinese).

    Google Scholar

    [15] Henan Institute of Geological Survey. 2009. Mineral prospect survey of Lushi area, Henan Province[R]. Zhengzhou (in Chinese).

    Google Scholar

    [16] Hu YX. 1986. Early Ordovician Microfossils and their stratigraphic significance in Gaoqiao area, Ziyang, Shaanxi[J]. Xi’an Institute of Geology and Mineral Resources, Chinese Academy of Geological Sciences, 14: 199−233 (in Chinese).

    Google Scholar

    [17] Huo LX, Song CZ. 2008. Tectonic deformation and simulation of Luanchuan Fault Zone[J]. Journal of Hefei University of Technology, 31(11): 1731−1735 (in Chinese with English abstract).

    Google Scholar

    [18] Johnson N G. 1985. Early Silurian Palynomorphs from the Tuscarora Fromation in central Pennsylvania and their paleobotanical and geological significance[J]. Review of Palaeobotany and Palynology[J]. Palynology, 45(3-4): 307-359. doi: 10.1016/0034-6667(85)90006-5.

    Google Scholar

    [19] Jia CZ, Shi YS, Guo LZ. 1988. East Qinling plate tectonics[M]. Nanjing: Nanjing University Press, 1–130 (in Chinese).

    Google Scholar

    [20] Li CD, Zhao LG, Xu YW, Chang QS, Wang SY, Xu T. 2018. Chronology of metasedimentary rocks from Kuanping Group Complex in North Qinling Belt and its geological significance[J]. Geology in China, 45(5): 992−1010 (in Chinese with English abstract).

    Google Scholar

    [21] Luo MJ, Zhang FM, Dong QY, Xu YR, Li SM, Li KH. 1991. China Molybdenum deposit[J]. Zhengzhou: Henan Science and Technology Press, 329 – 351 (in Chinese).

    Google Scholar

    [22] Lu LC. 1987. Suspected sources of the Arenigian formation in Huanghuachang, Yichang, Hubei[J]. Chinese Journal of Microbodies Paleontology, 4: 87−102 (in Chinese).

    Google Scholar

    [23] Lu SN, Li HK, Chen ZH, Hao GJ, Zhou HY, Guo JJ, Niu GH, Xiang ZQ. 2003. Geological evolution of the Middle Neoproterozoic Qinling Mountains and its response to the Rodinia supercontinent Event[M]. Beijing: Geological Press, 120–131 (in Chinese).

    Google Scholar

    [24] Lu SN, Yu HF, Li HK. 2009. Precambrian Geology of central orogenic Belt (Midwest) [M]. Beijing: Geological Press, 165–168 (in Chinese with English abstract).

    Google Scholar

    [25] Mao JW, Xie GQ, Yuan SD, Liu P, Meng XY, Zhou ZH, Zheng W. 2018. Current research progress and future trends of porphyry-skarn copper and granite-related tin polymetallic deposits in the Circum Pacific metallogenic belts[J]. Acta Petrologica Sinica, 34(9): 611−618 (in Chinese with English abstract).

    Google Scholar

    [26] Qinling Geological Team of Henan Bureau of Geo-exploration & Mineral Development. 1958. 1∶200 000-scale geological survey report of Luanchuan map-sheet (I49-XXⅡ)[R]. Zhengzhou (in Chinese).

    Google Scholar

    [27] Regional Geological Survey Team of the Department of Geology and Mineral Resources of Henan Province. 1995. 1∶50 000-scale regional geological survey report of Hengjian and Zhuyangguan map-sheets, Henan Province[R]. Pingdingshan

    Google Scholar

    [28] Ren JD, Lv JG, Zhang YX, Chao HL, Xie CY, Li CY, Li YQ, He CG, Wang XJ, Li RQ, Zhai WJ, Jiao JH, Sun XJ, Li M, Liu SS. 2020. 1∶50 000 Geological Map Database of Sanchuan Map-sheet, Henan Province[DB/OL]. Geoscientific Data & Discovery Publishing System. (2020-06-30). DOI: 10.35080/data.A.2020.P16.

    Google Scholar

    [29] Shanxi Geology and Mineral Bureau. 1989. Regional Geology of Shanxi province[M]. Beijing: Geology Press, 1–698 (in Chinese).

    Google Scholar

    [30] Sheng ZL, Luo MJ, Li LJ. 1980. Basic geological characteristics and main metallogenic control factors of Molybdenum ore belt in western Henan province[J]. Acta Geologica Sinica, 4(4): 300−309 (in Chinese with English abstract).

    Google Scholar

    [31] Shi QZ, Tao ZQ, Pang JQ, Qu MX. 1996. Study on Luanchuan Group at the southern margin of the North China Plate[J]. North China Journal of Geology and Mineral Resources, 11(1): 52−59 (in Chinese).

    Google Scholar

    [32] Song CZ, Zhang GW. 1999. The Funiushan nappe structure and its dynamic control[J]. Geological Review, 45(5): 492−497 (in Chinese).

    Google Scholar

    [33] Song CZ, Ren SL, Li JH, Chen ZC, Lian Y, Cai ZC. 2009. The strain partition in the southern margin of the North China plate: A study of Luonan-Luanchuan fault belt and the strong deformation belt in the northern margin of the Qinling orogenic belt[J]. Earth Science Frontiers, 16(3): 181−189 (in Chinese with English abstract).

    Google Scholar

    [34] Timofeev BV. 1973. Proterozoic and Early Palaeozoic microfossils[C]. Proceedings of the Third International Palynological Conference, Nauk, Moscow. 7–12.

    Google Scholar

    [35] Tianjin Center of China Geological Survey. 2015. Result report of regional geological survey of key areas of West Henan Province[R]. Tianjin (in Chinese).

    Google Scholar

    [36] Tianjin Center of China Geological Survey. 2019. Report of geological survey and result integration of key areas of Zhongtiao Mountain–Xiong’er Mountain metallogenic area[R]. Tianjin (in Chinese).

    Google Scholar

    [37] Wang S, Ye HS, Yang YQ, Zhang XK, Su HM, Yang CY. 2016. Zircon U-Pb Chronology, Geochemistry and Hf Isotopic Compositions of the Huoshenmiao Pluton, Western Henan[J]. Earth Science, 41(2): 293−316 (in Chinese with English abstract).

    Google Scholar

    [38] Wang ZQ, Gao LD, Wang T, Jiang CF. 2007. Microbody fossils found in The Taowan Group of Northern Qinling And their definition of stratigraphic age[J]. Science in China (Series D: Earth Sciences), 37(11): 1467−1473 (in Chinese with English abstract).

    Google Scholar

    [39] Wang ZQ, Yan QR, Yan Z, Wang T, Jiang CF, Gao LD. 2009. New division of major geotectonic units in the Qinling orogenic Belt[J]. Acta Geologica Sinica, 83(11): 1527−1546 (in Chinese with English abstract).

    Google Scholar

    [40] Yan GH, Cai JH, Ren KX, He GQ, Mou BL, Xu BL, Li FT, Yang B. 2007. Extensional magmatism in the North China Cratone Plate and the deep Earth dynamics of three supercontinents cracking[J]. Journal of Geology of Colleges and Universities, 13(2): 161−174 (in Chinese with English abstract).

    Google Scholar

    [41] Yan QR, Wang ZQ, Yan Z, Wang T, Chen JL, Xiang ZJ, Zhang Zq, Jiang CF. 2008. Genesis, age and tectonic significance of metamorphic mafic rocks of bandongping group in the Qinling Orogenic Belt[J]. Geological Bulletin, 27(9): 1475−1492 (in Chinese with English abstract).

    Google Scholar

    [42] Yang Y, Chen YJ, Zhang J, Zhang C. 2013. Ore geology, fluid inclusions and four-stage hydrothermal mineralization of the Shangfanggou giant Mo-Fe deposit in Eastern Qinling, central China[J]. Ore Geology Reviews, 55: 146−161. doi: 10.1016/j.oregeorev.2013.05.007

    CrossRef Google Scholar

    [43] Yang Y, Liu ZJ, Deng XH. 2017. Mineralization mechanisms in the Shangfanggou giant porphyry-skarn Mo-Fe deposit of the east Qinling, China: Constraints from H-O-C-S-Pb isotopes[J]. Ore Geology Reviews, 81(P2): 535−547.

    Google Scholar

    [44] Ye HS, Mao JW, Li YF, Yan CH, Guo YH, Zhao CS, He CF, Zheng RF, Chen L. 2006. Geological characteristics and metallogenic mechanism of molybdenum, tungsten, lead, zinc and silver deposits in Nihu ore field, Southwestern Henan Province[J]. Modern Geology, 20(1): 165−174 (in Chinese with English abstract).

    Google Scholar

    [45] Zhang GW, Yuan XC, Zhang BR, Xiao QH. 2001. Qinling orogenic belt and continental dynamics[M]. Beijing: Science Press, 1–885 (in Chinese with English abstract).

    Google Scholar

    [46] Zhang H, Gao LZ, Zhou HR, Song B, Ding XZ, Zhang CH, Liu HG, Gong CQ. 2019. Chronology progress of the Guandaokou and Luoyu groups in the southern margin of North China Craton: Constraints on zircon U-Pb dating of tuff by means of the SHRIMP[J]. Acta Petrologica Sinica, 35(8): 2470−2486 (in Chinese with English abstract). doi: 10.18654/1000-0569/2019.08.10

    CrossRef Google Scholar

    [47] Zhang SG, Wan YS, Liu GH, Cong YX, Zhao ZR. 1991. Metamorphic geology of Kuanping Group, North Qinling mountains[M]. Beijing: Beijing Science and Technology Press, 1–223 (in Chinese).

    Google Scholar

    [48] Zhang ZQ, Zhang Q. 1995. Geochemical characteristics of metamorphic basic volcanic rocks in the Late Proterozoic Kuanping ophiolite in the Northern Qinling Mountains[J]. Acta Petrologica Sinica, 11(Supp): 165−177 (in Chinese).

    Google Scholar

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