Meso-Cenozoic Asthenosphere Upwelling of Eastern China and Its Impacts on Structure-Magma-Mineralization Concentration Region
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摘要: 以深部地球物理资料为基础, 结合大地构造环境、岩浆岩同位素示踪及矿产资源分布规律, 加以综合分析.通过热力学计算可知, 中国东部近2亿年来的上地幔岩石圈/软流圈构造可以存留至今, 且能区分出中、新生代.软流圈上涌与矿集区：（1）中生代金属矿：（a）克拉通区, 软流圈沿柱身上涌, 其柱头上方形成幔壳混熔花岗质岩及相应Au、Cu、Mo、Pb-Zn等矿集区, 并于柱身与岩石圈块体陡接触带, 形成中基性杂岩及相应富Fe矿集区; （b）褶皱带区, 在软流圈上涌柱上方形成近幔源型花岗质岩, 相应为Cu、Au、Pb-Zn、Mo、Ag矿集区; （c）南岭带, 软流圈层在适当深度、热量充足、较大范围内"平卧", 因热传导而致使地壳内物质部分重熔, 形成壳源型花岗质岩及相应的W、Sn、稀有元素矿集区; （2）新生代油气田：（a）与太平洋板块俯冲有关的软流圈上涌, 其上方出露玄武岩, 形成较大型油田; （b）与裂陷盆地有关的软流圈上涌, 其上方形成大型油田, 也有中小型油田.软流圈上涌与大地构造：中生代J-K时期, 通过构造力特征等的综合分析, 阐明燕山运动的根源及其影响; 新生代侧重剖析大陆裂谷相关特征.总之, 软流圈上涌是岩石圈减薄, 以及中、新生代构造-岩浆-矿集区形成的根源.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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图 2 中国东部(大陆)岩石圈/软流圈构造图
据邢集善等(2009)修编
Fig. 2. Structure of lithosphere/asthenosphere of eastern China (mainland)
图 3 华北地震层折成象115°E南北向剖面
据邢作云等(2006a, 2006b)修编
Fig. 3. Seismic tomographic image along 115°E S-N section of North China
图 4 华南地震层析成像HW9东西向剖面
据邢集善等(2009)修编
Fig. 4. Seismic tomographic image along HW9 E-W section of South China
图 5 华南地震层析成像HW5东西向剖面
据邢集善等(2009)修编
Fig. 5. Seismic tomographic image along HW5 E-W section of South China
图 6 华北地震层析成像沿38.7°N东西向剖面
据邢作云等(2006a, 2000b)修编
Fig. 6. Seismic tomographic image along 38.7°N E-W section of North China
图 7 东北地区东乌旗-大兴安岭(南)-丹东大地电磁测深剖面
据国家地震局(1992)修编
Fig. 7. Magnetotelluric sounding profile of Dongwuqi-Daxing'anling (south)-Dandong in Northeast China
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[1] Changchun University of Geology, 1998.Manzhouli-Suifenhe Geoscience Transects of China.Geological Publishing House, Bejing (in Chinese). [2] Chen, Y.C., 1999.The Prospective Evaluation of Mineral Resources in the Main Metallogenic Regions in China.Geological Publishing House, Beijing (in Chinese). [3] China Seismological Bureau, 1992.Explanation of GGT from Dongwuzhumuqinqi of Inner Mongolia to Donggou of Liaoning Province.Seismological Press, Beijing (in Chinese). [4] 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 [5] 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 [6] 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). [7] 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). [8] 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 [9] 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 [10] 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 [11] 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 [12] 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 [13] 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). [14] 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 [15] 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). [16] 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). [17] 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 [18] 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). [19] 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). [20] 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). [21] 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). [22] Ma, X.Y., 1987.The Lithosphere Geodynamics Compendium in China.Geological Publishing House, Beijing (in Chinese). [23] 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 [24] 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). [25] Pei, R.F., Zhai, Y.S., Zhang, B.R., et al., 1999.Deep-Seated Tectonism and Mineralization.Geological Publishing House, Beijing (in Chinese). [26] Ren, J.S., 2000.The Tectonic Map of China and Neighbour Area.Geological Publishing House, Beijing (in Chinese). [27] 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). [28] 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 [29] Wang, J.Y., 1990.Compilation of the Chinese Continental Geothermal Value Data.Seismology and Geology, 12(4):351-363 (in Chinese with English abstract). [30] 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). [31] 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). [32] 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 [33] Xiao, Q.H., Deng, J.F., Ma, D.Q., et al., 2002.The Way of Investigation on Granitoids.Geological Publishing House, Beijing (in Chinese). [34] 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). [35] 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 [36] 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). [37] 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). [38] 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). [39] 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). [40] 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 [41] 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). [42] 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). [43] Yang, W.R., 2004.Some Problems of Opening-Closing Tectonics.Geological Bulletin of China, 23(3):195-199 (in Chinese with English abstract). [44] 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 [45] Yuan, X.C., 1996.Atlas of Geophysics of China.Geological Publishing House, Beijing (in Chinese). [46] Zhai, Y.S., Deng, J., Li, X.B., 1999.Essentials of Metallogeny.Geological Publishing House, Beijing (in Chinese). [47] Zhai, Y.S., Zhang, H., Song, H.L., et al., 1997.Large Structure and Superlarge Deposit.Geological Publishing House, Beijing (in Chinese). [48] 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. [49] 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). [50] 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. [51] 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. [52] 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. [53] 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 [54] 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 [55] 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. [56] 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 [57] 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 [58] 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 [59] 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 [60] 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 [61] 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 [62] 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. [63] 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 [64] 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 [65] 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 [66] 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 [67] 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 [68] 马杏垣, 1987.中国岩石圈动力学纲要.北京:地质出版社. [69] 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 [70] 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 [71] 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. [72] 任纪舜, 2000.中国及邻区大地构造图.北京:地质出版社. [73] 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 [74] 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 [75] 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 [76] 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 [77] 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 [78] 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 [79] 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. [80] 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 [81] 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 [82] 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 [83] 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 [84] 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. [85] 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. [86] 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 [87] 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. [88] 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 [89] 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 [90] 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 [91] 袁学诚, 1996.中国地球物理图集.北京:地质出版社. [92] 翟裕生, 邓军, 李小波, 1999.区域成矿学.北京:地质出版社. [93] 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. [94] 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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