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    Volume 44 Issue 5
    May  2019
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    Article Navigation >  Earth Science  > 2019  >  44(5): 1570-1583
    Xing Jishan, Yang Weiran, Xing Zuoyun, Liu Jianhua, 2019. Meso-Cenozoic Asthenosphere Upwelling of Eastern China and Its Impacts on Structure-Magma-Mineralization Concentration Region. Earth Science, 44(5): 1570-1583. doi: 10.3799/dqkx.2019.976
    Citation: Xing Jishan, Yang Weiran, Xing Zuoyun, Liu Jianhua, 2019. Meso-Cenozoic Asthenosphere Upwelling of Eastern China and Its Impacts on Structure-Magma-Mineralization Concentration Region. Earth Science, 44(5): 1570-1583. doi: 10.3799/dqkx.2019.976
    shu

    Meso-Cenozoic Asthenosphere Upwelling of Eastern China and Its Impacts on Structure-Magma-Mineralization Concentration Region

    doi: 10.3799/dqkx.2019.976
    • 1.

      Geophysical and Geochemical Prospecting Institute, Shanxi Provincial Geological Prospecting Bureau, Yuncheng 044004, China

    • 2.

      School of Earth Sciences, China University of Geosciences, Wuhan 430074, China

    • 3.

      Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

    • Received Date: 2019-02-20
    • Publish Date: 2019-05-15
      Abstract
    • Based on the deep geophysical data, a comprehensive study is carried out by analyzing the tectonic environment, magma isotopic tracing and laws of distribution of mineral resources. The thermodynamic calculation indicates that the structure of the upper mantle lithosphere and asthenosphere of the eastern China which is near 200 Ma can be kept to now, and the time of Mesozoic and Cenozoic can be recognized. Results show the following asthenosphere upwelling and mineralization concentration regions. (1) Mesozoic metal deposit:(a) Craton area, asthenosphere upwelled along the plume body, above the plume head, there formed intermingling granitic rock of crust and mantle melts and corresponding Au, Cu, Mo, Pb-Zn etc mineralization concentrated region. And in the steep contact belt of the plume body and lithosphere body, there formed mediate-basic complex and corresponding Fe mineralization concentrated region. (b) Fold belt area, above the asthenosphere upwelling plume, there formed near mantle-source granitic rocks, and corresponding Cu, Au, Pb-Zn, Mo, Ag mineralization concentrated region. (c) Nanling belt, asthenosphere was "recumbent" at suitable depth, with adequate heat and to a great extent, for heat conduction, the interior of crust remelted partially, and the crust-source granitic rocks, corresponding W, Sn and rare elements mineralization concentrated regions were formed. (2) Cenozoic oil and gas field:(a) Asthenosphere upwelling related with the Pacific subduction, above them, there outcropped basalt, and formed large-scale oil field. (b) Asthenosphere upwelling related with the rift basin, above them, there formed large-scale oil fields, also medium- and small-scale oil fields. Asthenosphere upwelling and tectonic:at J-K of Mesozoic, through comprehensive analysis of tectonic force etc, the origin and influence of Yanshan movement are presented. For Cenozoic, the characters related with continental rift should be analyzed essentially. In conclusion, asthenosphere upwelling is the origin of lithosphere thinning and formation of Meso-Cenozoic structure-magma-mineralization concentration region.

       

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      • References(94)
    • Changchun University of Geology, 1998.Manzhouli-Suifenhe Geoscience Transects of China.Geological Publishing House, Bejing (in Chinese).
      Chen, Y.C., 1999.The Prospective Evaluation of Mineral Resources in the Main Metallogenic Regions in China.Geological Publishing House, Beijing (in Chinese).
      China Seismological Bureau, 1992.Explanation of GGT from Dongwuzhumuqinqi of Inner Mongolia to Donggou of Liaoning Province.Seismological Press, Beijing (in Chinese).
      Deng, J.F., Mo, X.X., Zhao, H.L., et al., 1999.The Yanshanian Lithosphere-Asthenosphere Catastrophe and Metallogenic Environment in East China.Mineral Deposits, 18(4):309-315 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kcdz199904003
      Deng, J.F., Su, S.G., Zhao, H.L., et al., 2003.Deep Processes of Mesozoic Yanshanian Lithosphere Thinning in North China.Earth Science Frontiers, 10(3):41-50 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy200303003
      Deng, J.F., Teng, J.W., Peng, C., et al., 2008.Features and Deep Geology of Geophysical Field and Mineralization in China.Geological Publishing House, Beijing (in Chinese).
      He, L.J., Hu, S.B., Wang, J.Y., 2001.Heat Lithosphere Structural Characteristics of Eastern China Continent.Progress in Natural Science, 11(9):966-969 (in Chinese).
      Hong, D.W., Wang, T., Tong, Y., et al., 2003.Mesozoic Granitoids from North China Block and Qinling-Dabie-Sulu Orogenic Belt and Their Deep Dynamic Process.Earth Science Frontiers, 10(3):231-256 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dxqy200303022
      Hua, R.M., Chen, P.R., Zhang, W.L., et al., 2005.Three Major Metallogenic Events in Mesozoic in South China.Mineral Deposits, 24(2):99-107 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kcdz200502002
      Huang, J., Zhao, D., 2006.High-Resolution Mantle Tomography of China and Surrounding Regions.Journal of Geophysical Research (Solid Earth), 111(B9):396. https://doi.org/10.1029/2005JB004066
      Lehedev, S., Nolet, G., 2003.Upper Mantle beneath Southeast Asia from S Velocity Tomography.Journal of Geophysical Research (Solid Earth), 108(B1):165. https://doi.org/10.1029/2000JB000073
      Li, C., Robert, V.H., Nafl, T.M., 2006.Constraining P-Wave Velocity Variations in the Upper Mantle beneath Southeast Asia.Phys.Earth Planet.Inter., 154:180-195. doi: 10.1016/j.pepi.2005.09.008
      Li, C., Wang, L.S., Shi, Y.S., 1996.Deep Thermal State and Lithospheric Thickness in the Lower Yangtze Area.Journal of Nanjing University (Natural Sciences), 32(3):494-499 (in Chinese with English abstract).
      Li, T.D., 2006.Lithospheric Tectonic Units of China.Geology in China, 33(4):700-710 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dqwlxb201801013
      Liu, F.T., Qu, K.X., Wu, H., et al., 1986.ST Image of North China.Acta Geoscientica Sinica, 29(5):442-449 (in Chinese with English abstract).
      Liu, G.D., 1985.Cenozoic Rift System of North China Plain and the Deep Internal Processes.In: Research on Crustal Movement (1).Seismological Press, Beijing, 17-25 (in Chinese with English abstract).
      Liu, H.F., Liang, H.S., Li, X.Q., et al., 2000.The Coupling Mechanisms of Mesozoic-Cenozoic Rift Basins and Extensional Mountain System in Eastern China.Earth Science Frontiers, 7(4):477-486 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy200004015
      Liu, J.H., Liu, F.T., Wu, H., et al., 1989.Three Dimensional Velocity Images of the Crust and Upper Mantle beneath North-South Zone in China.Acta Geoscientica Sinica, 32(2):143-152 (in Chinese with English abstract).
      Liu, J.H., Liu, F.T., Yan, X.W., et al., 2004.A Study of Lg Coda Attenuation beneath North China:Seismic Imaging Lg Coda Q.Chinese Journal Geophysics, 47(5):822-832 (in Chinese with English abstract).
      Liu, J.H., Wu, H., Liu, F.T., 1996.Features of 3-D Velocity Distribution and Lithosphere Structure in South China and Its Contiguous Sea Area.Acta Geoscientica Sinica, 39(4):483-492 (in Chinese with English abstract).
      Lu, F.X., Zheng, J.P., Hou, Q.Y., et al., 2006.Zones of Crust-Mantle and Lithosphere-Asthenosphere Interaction in Eastern China:Characteristics and Timing of Transformation.Geology in China, 33(4):773-781 (in Chinese with English abstract).
      Ma, X.Y., 1987.The Lithosphere Geodynamics Compendium in China.Geological Publishing House, Beijing (in Chinese).
      Mao, J.W., Xie, G.Q., Li, X.F., et al., 2004.Mesozoic Large Scale Mineralization and Multiple Lithospheric Extension in South China.Earth Science Frontiers, 11(1):45-55 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy200401003
      Mao, J.W., Xie, G.Q., Zhang, Z.H., et al., 2005.Mesozoic Large-Scale Metallogenic Pulses in North China and Corresponding Geodynamic Settings.Acta Petrologica Sinica, 21(1):169-188 (in Chinese with English abstract).
      Pei, R.F., Zhai, Y.S., Zhang, B.R., et al., 1999.Deep-Seated Tectonism and Mineralization.Geological Publishing House, Beijing (in Chinese).
      Ren, J.S., 2000.The Tectonic Map of China and Neighbour Area.Geological Publishing House, Beijing (in Chinese).
      Shao, J.A., Liu, F.T., Chen, H., et al., 2001.Relationship between Mesozoic Magmatism and Subduction in Da Hinggan-Yanshan Area.Acta Geologica Sinica, 75(1):56-63 (in Chinese with English abstract).
      Wang, D.Z., Shen, W.Z., 2003.Genesis of Granitoids and Crustal Evolution in Southeast China.Earth Science Frontiers, 10(3):209-220 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy200303020
      Wang, J.Y., 1990.Compilation of the Chinese Continental Geothermal Value Data.Seismology and Geology, 12(4):351-363 (in Chinese with English abstract).
      Wang, L.S., Li, C., Shi, Y.S., et al., 1995.Distributions of Geotemperature and Terrestrial Heat Flow Density in Lower Yangtze Area.Acta Geoscientica Sinica, 38 (4):469-476 (in Chinese with English abstract).
      Wang, Q., Xu, J.F., Zhao, Z.H., et al., 2003.Petrogenesis of the Mesozoic Intrusive Rocks in the Tongling Area, Anhui Province, China and Their Constraint on Geodynamic Process.Science in China (Series D:Earth Sciences), 33(4):323-334 (in Chinese).
      Wei, W.B., Jin, S., Ye, G.F., et al., 2006.MT Sounding and Lithosphere Thickness in North China.Geology in China, 33(4):762-772 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi200604006
      Xiao, Q.H., Deng, J.F., Ma, D.Q., et al., 2002.The Way of Investigation on Granitoids.Geological Publishing House, Beijing (in Chinese).
      Xiao, Q.H., Qiu, R.Z., Deng, J.F., et al., 2005.Granitoids and Continental Crustal Growth Modes in China.Geology in China, 32(3):343-352 (in Chinese with English abstract).
      Xiao, Q.H., Qiu, R.Z., Wu, G.Y., et al., 2006.Mesozoic Asthenospheric Upwelling Orogeny in Eastern China.Geology in China, 33(4):730-750 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi200604004
      Xing, J.S., Liu, J.H., Zhao, J.Q., 2002.Deep-Seated Tectonics in the North China Intraplate.Earthquake Research in Shanxi, (4):3-12 (in Chinese with English abstract).
      Xing, J.S., Yang, W.R., Xing, Z.Y., et al., 2007.Deep-Seated Structure Characteristics of Eastern China and Its Relation with Metal Mineralization-Concentrated Region.Earth Science Frontiers, 14(3):114-130 (in Chinese with English abstract).
      Xing, J.S., Yang, W.R., Xing, Z.Y., et al., 2009.Mesozoic Asthenosphere Upwelling of Eastern China and Its Effects on Structure-Magma-Mineralization-Concentrated Region.Earth Science Frontiers, 16(4):225-239 (in Chinese with English abstract).
      Xing, Z.Y., 2007.Deep-Seated Structural Characteristics of North China and Its Near-Surface Response (Dissertation). China University of Geosciences, Beijing (in Chinese with English abstract).
      Xing, Z.Y., Xing, J.S., Zhao, B., 2006a.Deep-Seated Structure of North China.Geological Science and Technology Information, 25(6):17-23, 36 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201803017
      Xing, Z.Y., Xing, J.S., Zhao, B., et al., 2006b.Identification of Deep Structure of Two Episodes in North China and Its Significance—Yanshanian Movement and Deep Process.Geological Review, 52(4):433-441, 578 (in Chinese with English abstract).
      Xing, Z.Y., Zhao, B., Tu, M.Y., et al., 2005.The Formation of the Fenwei Rift Valley.Earth Science Frontiers, 12(2):247-262 (in Chinese with English abstract).
      Yang, W.R., 2004.Some Problems of Opening-Closing Tectonics.Geological Bulletin of China, 23(3):195-199 (in Chinese with English abstract).
      Yang, W.R., Zeng, Z.X., Li, D.W., et al., 2009.Three-Level Tectonic Model for Intraplate Earthquakes.Earth Science Frontiers, 16(1):206-217 (in Chinese with English abstract). doi: 10.1016/S1872-5791(08)60073-1
      Yuan, X.C., 1996.Atlas of Geophysics of China.Geological Publishing House, Beijing (in Chinese).
      Zhai, Y.S., Deng, J., Li, X.B., 1999.Essentials of Metallogeny.Geological Publishing House, Beijing (in Chinese).
      Zhai, Y.S., Zhang, H., Song, H.L., et al., 1997.Large Structure and Superlarge Deposit.Geological Publishing House, Beijing (in Chinese).
      Zhao, D.P., Yamada, A., Hta, Y.O., 2006.Precisely Measured Travel Times of Mantle Body Waves:Implications for Mantle Heterogeneity and Tomography.Earth Science Frontiers, 13(2):37-47.
      Zhao, Y.G., Zhong, D.L., Liu, J.H., et al., 1992.Fundamentals of Geological Interpretation for Seismic Tomography and Its Application to Studying of West Yunnan's Deep Structure.Scientia Geologica Sinica, 27(2):105-113 (in Chinese with English abstract).
      长春地质学院, 1998.中国满洲里-绥芬河地学断面.北京:地质出版社.
      陈毓川, 1999.中国主要成矿区带矿产资源远景评价.北京:地质出版社.
      国家地震局, 1992.内蒙古东乌珠穆沁旗至辽宁东沟地学断面说明书.北京:地震出版社.
      邓晋福, 莫宣学, 赵海玲, 等, 1999.中国东部燕山期岩石圈-软流圈系统大灾变与成矿环境.矿床地质, 18(4):309-315. doi: 10.3969/j.issn.0258-7106.1999.04.003
      邓晋福, 苏尚国, 赵海玲, 等, 2003.华北地区燕山期岩石圈减薄的深部过程.地学前缘, 10(3):41-50. doi: 10.3321/j.issn:1005-2321.2003.03.003
      邓晋福, 滕吉文, 彭聪, 等, 2008.中国地球物理场特征及深部地质与成矿.北京:地质出版社.
      何丽娟, 胡圣标, 汪集旸, 2001.中国东部大陆地区岩石圈热结构特征.自然科学进展, 11(9):966-969. doi: 10.3321/j.issn:1002-008X.2001.09.013
      洪大卫, 王涛, 童英, 等, 2003.华北地区和秦岭-大别-苏鲁造山带中生代花岗岩与深部地球动力学过程.地学前缘, 10(3): 231-256. doi: 10.3321/j.issn:1005-2321.2003.03.022
      华仁民, 陈培荣, 张文兰, 等, 2005.论华南地区中生代3次大规模成矿作用.矿床地质, 24(2):99-107. doi: 10.3969/j.issn.0258-7106.2005.02.002
      李成, 王良书, 施央申, 1996.下扬子区深部热状态与岩石圈厚度.南京大学学报(自然科学版), 32(3):494-499. http://www.cnki.com.cn/Article/CJFDTOTAL-NJDZ603.019.htm
      李廷栋, 2006.中国岩石圈构造单元.中国地质, 33(4):700-710. doi: 10.3969/j.issn.1000-3657.2006.04.002
      刘福田, 曲克信, 吴华, 等, 1986.华北地区地震层面成像.地球物理学报, 29(5):442-449. doi: 10.3321/j.issn:0001-5733.1986.05.003
      刘国栋, 1985.华北平原新生代裂谷系及其深部过程.见: 现代地壳运动研究(1).北京: 地震出版社, 17-25.
      刘和甫, 梁慧社, 李晓清, 等, 2000.中国东部中新生代裂陷盆地与伸展山岭耦合机制.地学前缘, 7(4):477-486. http://d.old.wanfangdata.com.cn/Periodical/dxqy200004017
      刘建华, 刘福田, 吴华, 等, 1989.中国南北带地壳和上地幔的三维速度图像.地球物理学报, 32(2):143-152. doi: 10.3321/j.issn:0001-5733.1989.02.003
      刘建华, 刘福田, 阎晓蔚, 等, 2004.华北地区Lg尾波衰减研究——Lg尾波Q的测量.地球物理学报, 47(5):822-832. doi: 10.3321/j.issn:0001-5733.2004.05.013
      刘建华, 吴华, 刘福田, 1996.华南及其海域三维速度分布特征与岩石层结构.地球物理学报, 39(4):483-492. doi: 10.3321/j.issn:0001-5733.1996.04.006
      路凤香, 郑建平, 侯青叶, 等, 2006.中国东部壳-幔、岩石圈-软流圈之间的相互作用带:特征及转换时限.中国地质, 33(4):773 -781. doi: 10.3969/j.issn.1000-3657.2006.04.007
      马杏垣, 1987.中国岩石圈动力学纲要.北京:地质出版社.
      毛景文, 谢桂青, 李晓峰, 等, 2004.华南地区中生代大规模成矿作用与岩石圈多阶段伸展.地学前缘, 11(1):45-54. doi: 10.3321/j.issn:1005-2321.2004.01.003
      毛景文, 谢桂青, 张作衡, 等, 2005.中国北方中生代大规模成矿作用的期次及其地球动力学背景.岩石学报, 21(1):169-188. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200501017
      裴荣富, 翟裕生, 张本仁, 等, 1999.深部构造作用与成矿.北京:地质出版社.
      任纪舜, 2000.中国及邻区大地构造图.北京:地质出版社.
      邵济安, 刘福田, 陈辉, 2001.大兴安岭-燕山晚中生代岩浆活动与俯冲作用的关系.地质学报, 75(1):56-63. doi: 10.3321/j.issn:0001-5717.2001.01.006
      王德滋, 沈渭洲, 2003.中国东南部花岗岩成因与地壳演化.地学前缘, 10(3):209-220. doi: 10.3321/j.issn:1005-2321.2003.03.020
      汪集旸, 1990.中国大陆地区大地热流值数据汇编.地震地质, 12(4):351-363. http://www.cnki.com.cn/Article/CJFDTOTAL-DQWX201608015.htm
      王良书, 李成, 施央申, 等, 1995.下扬子区地温场和大地热流密度分布.地球物理学报, 38(4):469-476. doi: 10.3321/j.issn:0001-5733.1995.04.007
      王强, 许继峰, 赵振华, 等, 2003.安徽铜陵地区燕山期侵入岩的成因及其对深部动力学过程的制约.中国科学(D辑:地球科学), 33(4):323-334. http://d.old.wanfangdata.com.cn/Periodical/zgkx-cd200304005
      魏文博, 金胜, 叶高峰, 等, 2006.华北地区大地电磁测深及岩石圈厚度讨论.中国地质, 33(4):762-772. doi: 10.3969/j.issn.1000-3657.2006.04.006
      肖庆辉, 邓晋福, 马大拴, 等, 2002.花岗岩研究思维与方法.北京:地质出版社.
      肖庆辉, 邱瑞照, 邓晋福, 等, 2005.中国花岗岩与大陆地壳生长方式初步研究.中国地质, 32(3):343-352. http://d.old.wanfangdata.com.cn/Periodical/zgdizhi200503001
      肖庆辉, 邱瑞照, 伍光英, 等, 2006.中国东部中生代软流层上涌造山作用.中国地质, 33(4):730-750. doi: 10.3969/j.issn.1000-3657.2006.04.004
      邢集善, 刘建华, 赵晋泉, 2002.华北板内深部构造.山西地震, (4):3-12. doi: 10.3969/j.issn.1000-6265.2002.04.002
      邢集善, 杨巍然, 邢作云, 等, 2007.中国东部深部构造特征及其与矿集区关系.地学前缘, 14(3):114-130. doi: 10.3321/j.issn:1005-2321.2007.03.010
      邢集善, 杨巍然, 邢作云, 等, 2009.中国东部中生代软流圈上涌与构造-岩浆-矿集区.地学前缘, 16(3):225-239.
      邢作云, 2007.华北地区深部构造特征及其浅表响应(博士学位论文).北京: 中国地质大学.
      邢作云, 邢集善, 赵斌, 2006a.华北地区深部构造特征.地质科技情报, 25(6):17-23, 36. http://d.old.wanfangdata.com.cn/Periodical/dzkjqb200606003
      邢作云, 邢集善, 赵斌, 等, 2006b.华北地区两个世代深部构造的识别及其意义——燕山运动与深部过程.地质论评, 52(4):433-441, 578.
      邢作云, 赵斌, 涂美义, 等, 2005.汾渭裂谷系与造山带耦合关系及其形成机制研究.地学前缘, 12(2):247-262. doi: 10.3321/j.issn:1005-2321.2005.02.027
      杨巍然, 2004.开合构造研究中的几个问题.地质通报, 23(3):195-199. doi: 10.3969/j.issn.1671-2552.2004.03.004
      杨巍然, 曾佐勋, 李德威, 等, 2009.板内地震过程的三层次构造模式.地学前缘, 16(1):206-217. doi: 10.3321/j.issn:1005-2321.2009.01.023
      袁学诚, 1996.中国地球物理图集.北京:地质出版社.
      翟裕生, 邓军, 李小波, 1999.区域成矿学.北京:地质出版社.
      翟裕生, 张湖, 宋鸿林, 等, 1997.大型构造与超大型矿床.北京:地质出版社.
      赵永贵, 钟大赍, 刘建华, 等, 1992.地震层析地质解释原理及其在滇西深部构造研究中的应用.地质科学, 27(2):105-113.
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