[1] Chen, N.S., Wang, X.Y., Zhang, H.F., et al., 2007. Geochemistry and Nd-Sr-Pb Isotopic Compositions of Granitoids from Qaidam and Oulongbuluke Micro-Blocks, NW China: Constraints on Basement Nature and Tectonic Affinity. Earth Science, 32(1): 7-21(in Chinese with English abstract). http://cn.bing.com/academic/profile?id=a71631285a6f30cfadd12e61f77d4c4c&encoded=0&v=paper_preview&mkt=zh-cn
[2] Chen, S., Li, X.P., Kong, F.M., et al., 2018. Metamorphic Evolution and Zircon U-Pb Ages of the Nanshankou Mafic High Pressure Granulites from the Jiaobei Terrane, North China Craton. Journal of Earth Science, 29(5): 1219-1235. https://doi.org/10.1007/s12583-017-0956-9
[3] Chen, W., Wan, Y.S., Li, H.Q., et al., 2011. Isotope Geochronology: Technique and Application. Acta Geologica Sinica, 85(11): 1917-1947(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/fxhx201703002
[4] Chen, X.Y., Li, H.Z., Lu, W.J., et al., 2011. Overview of Research Advances in Lamprophyre. Journal of the Graduates Sun Yat-Sen University(Natural Sciences, Medicine), 32(4): 21-29(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=8524623
[5] Chen, Y.C., Chang, Y.F., Pei, R.F., et al., 2007.China Metallogenic System and Regional Metallogenic Evaluation. Geological Publishing House, Beijing (in Chinese with English abstract).
[6] DePaolo, D.J., Wasserburg, G. J., 1976. Inferences about Magma Sources and Mantle Structure from Variations of 143Nd/144Nd. Geophysical Research Letters, 3(12): 743-746. https://doi.org/10.1029/gl003i012p00743
[7] Dupuy, C., Dostal, J., 1984. Trace Element Geochemistry of Some Continental Tholeiites. Earth and Planetary Science Letters, 67(1): 61-69. https://doi.org/10.1016/0012-821x(84)90038-4
[8] Faure, G., 1986.Principles of Isotope Geology. John Wiley and Sons, New York, 93-96.
[9] Guan, T., Huang, Z.L., Xie, L.H., et al., 2003. Geochemistry of Lamprophyres in Baimazhai Nickel Deposit, Yunnan Province, Ⅰ. Major and Trace Elements. Acta Mineralogica Sinica, 23(3): 278-288(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kwxb200303016
[10] Hart, S.R., Li, S.G., Zheng, S.G., et al., 1989.Timing of Collision between the North and South China Blocks—The Sm-Nd Isotopic Age Evidence. Science in China, 32(11):1393-1400. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=639b1c63668588712169cf07e016815a
[11] Hou, G.T., 2012.North China Basic Dyke Swarm. Science Press, Beijing(in Chinese).
[12] Hu, R.Z., Jin, J.F., 1990. The Origin of Lamprophyre in Guidong Granitic Complex. Mineralogy and Petrology, 10(4): 1-7(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KWYS199004001.htm
[13] Huang, Z.L., Liu, C.Q., Zhu, C.M., et al., 1999.Genesis of Lamprophyre in Laowangzhai Gold Deposit, Yunnan and Its Relationship with Gold Mineralization. Geological Publishing House, Beijing(in Chinese).
[14] Jacobsen, S. B., Wasserburg, G. J., 1980. Sm-Nd Isotopic Evolution of Chondrites. Earth and Planetary Science Letters, 50(1): 139-155. https://doi.org/10.1016/0012-821x(80)90125-9
[15] Li, S.C., Zhang, L.Y., Li, P.C., et al., 2017.Discovery and Tectonic Implications of Early Triassic O-Type Adakite in Middle of Great Xing'an Range.Earth Science, 42(12):2117-2128(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201712002
[16] Li, T., Ni, S.B., 1997. Element Abundances of the Continental Lithosphere in China. Geology and Prospecting, 33(1): 31-37(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=73a6c8b605c3deec63814f462655713c
[17] Li, X.H., Zhou, H.W., Wei, G.J., et al., 2002. Geochemistry and Sr-Nd Isotopes of Cenozoic Ultrapotassic Lamprophyres in Western Yunnan: Constraints on the Composition of Subcontinental Lithospheric Mantle. Geochimica, 31(1): 26-34(in Chinese with English abstract).
[18] Li, Y.J., Li, G.Y., Tong, L.L., et al., 2015.Discrimination of Ratios of Ta, Hf, Th, La, Zr and Nb for Tectonic Setting in Basalts. Journal of Earth Sciences and Environment, 37 (3): 14-21(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-XAGX201503004.htm
[19] Ling, H.F., Xu, S.J., Shen, W.Z., et al., 1998. Nd, Sr, Pb and O Isotopic Compositions of Late Proterozoic Gezong- and Donggu-Granites in the West Margin of Yangtze Plate and Comparison with Other Coeval Granitoids. Acta Petrologica Sinica, 14(3): 269-277(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98199803001
[20] Liu, S., Hu, R.Z., Feng, G.Y., et al., 2010. Distribution and Significance of the Mafic Dyke Swarms since Mesozoic in North China Craton. Geological Bulletin of China, 29(2-3): 259-267(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz201002010
[21] Liu, Z.H., Wu, X.B., 2009.Relationship between Meso-Basic Veins and Uranium Mineralization. Modern Mining, 25(3):77-80(in Chinese). http://cn.bing.com/academic/profile?id=317946ac0c5053c20433d1e70c6d641e&encoded=0&v=paper_preview&mkt=zh-cn
[22] Lu, L.X., Du, M., Shao, H.S., 2015. Comparison and Discussion of K-Ar and Ar-Ar Dating Methods. Liaoning Chemical Industry, 44(8): 1025-1027(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=lnhg201508041
[23] Lu, F.X., Shu, X.X., Zhao, C.H., 1991. A Suggestion on Classification of Lamprophyres. Geological Science and Technology Information, 10(Suppl.): 55-62(in Chinese with English abstract).
[24] Ma, C.Q., Li, Z. C., Ehlers, C., et al., 1998. A Post-Collisional Magmatic Plumbing System: Mesozoic Granitoid Plutons from the Dabieshan High-Pressure and Ultrahigh-Pressure Metamorphic Zone, East-Central China. Lithos, 45(1-4): 431-456. https://doi.org/10.1016/s0024-4937(98)00043-7
[25] Ma, Y.F., Liu, Y.J., Wen, Q.B., et al., 2017.Petrogenesis and Tectonic Settings of Volcanic Rocks from Late Triassic Hadataolegai Fm. at Central Part of Great Xing'an Range. Earth Science, 42(12):2146-2173(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201712004
[26] Menzies, M.A., 1983.Mantle Ultramafic Xenoliths in Alkaline Magmas: Evidence for Mantle Heterogeneity Modified by Magmatic Activity. In: Hawkesworth, C.J., Norry, M.J., eds., Continental Basalts and Mantle Xenoliths. Shiva, London, 92-110.
[27] Münker, C., 1998. Nb/Ta Fractionation in a Cambrian Arc/back Arc System, New Zealand: Source Constraints and Application of Refined ICPMS Techniques. Chemical Geology, 144(1-2): 23-45. https://doi.org/10.1016/s0009-2541(97)00105-8
[28] Song, X.Y., Qin, G.J., 1994.The Metallogenc Significance of Lamprophyre. Mineral Resources and Geology, 8(2): 81-87(in Chinese with English abstract).
[29] Rollison, H.R., 2000. Petro-Geochemistry(Yang, X.M., Yang, X.Y., Chen, S.X., Translated). Press of University of Science and Technology of China, Hefei, 186-187.
[30] Rong, J.S., Han, Z.H., Xia, Y.L., 1984.Granitic Pluton Type of Mineralization Characteristics of Uranium Deposits and Mineralization in China. Radioactive Geology, 2(2):1-11(in Chinese). http://d.old.wanfangdata.com.cn/Periodical/gxdzxb201802003
[31] Sun, J.G., Hu, S.X., Ling, H.F., et al., 2000. Element Geochemistry and Origin of High Potassic-Potassic Dike Rocks in Two Types of Goldfields in Northwest Jiaodong, Shandong, China. Geochimica, 29(2): 143-152(in Chinese with English abstract). http://cn.bing.com/academic/profile?id=cfbc7f91f0e59ad5274ea5b23062483f&encoded=0&v=paper_preview&mkt=zh-cn
[32] Sun, S.S., McDonough, W. F., 1989. Chemical and Isotopic Systematics of Oceanic Basalts: Implications for Mantle Composition and Processes. Geological Society, London, Special Publications, 42(1): 313-345. https://doi.org/10.1144/gsl.sp.1989.042.01.19
[33] Sun, Y., Li, J.C., Ding, J., et al., 2017. Characteristics and Genesis of Lamprophyre Vein Type Uranium Mineralization in the West of Mianning, Sichuan. Acta Geologica Sichuan, 37(2): 209-213(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=scdzxb201702008
[34] Tarney, J., Jones, C. E., 1994. Trace Element Geochemistry of Orogenic Igneous Rocks and Crustal Growth Models. Journal of the Geological Society, 151(5): 855-868. https://doi.org/10.1144/gsjgs.151.5.0855
[35] Taylor, S.R., McLennan, S.M., 1985.The Continental Crust: Its Composition and Evolution. Blackwell Scientific Publications, Oxford.
[36] Wang, Z.Q., Li, Z.Y., Zhang, G.Y., et al., 2007. Geochemical Characteristics and the Provenance of Cretaceous Basic Dikes in Zhongdong Area of Xiazhuang Uranium Ore Field. Uranium Geology, 23(4): 218-225, 248(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ykdz200704005
[37] Waxilali, Li, H.Z., Liang, J., et al., 2011. Review of the Species, Petrogenesis of Lamprophyre and Its Relationship with Mineralization. Journal of the Graduates Sun Yat-Sen University(Natural Sciences, Medicine), 32(4): 1-13(in Chinese with English abstract). http://cn.bing.com/academic/profile?id=c6e8caf65cb5594232ced58b71194c1d&encoded=0&v=paper_preview&mkt=zh-cn
[38] Xiao, C.D., Zhang, Z.L., Zhao, L.Q., 2004. Nd, Sr and Pb Isotope Geochemistry of Yanshanian Granitoids in Eastern Inner Mongolia and Their Origins. Geology in China, 31(1): 57-63(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi200401008
[39] Xin, C.L., Ma, W.Y., An, G.B., et al., 2013. Geological Characteristics and Mineralization Mechanism of the No.207 Uranium Deposit in Longshoushan, Gansu Province. Acta Geologica Sinica, 87(4): 577-590(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb201304011
[40] Xu, D.R., 2000. Relationship between Lamprophyre and Gold Mineralization in the Gezhen Gold-Bearing Shear Zone in Hainan Province. Geotectonica et Metallogenia, 24(3): 258-265(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ddgzyckx200003010
[41] Xu, J.F., Qiu, J.X., 1991.The Fractional Crystallization of Basaltic Magma in Shanwang, Shandong Province. Earth Science, 16(4):369-376(in Chinese with English abstract).
[42] Yang, C.S., Zhang, S.M., Zhao, Y.Y., et al., 2015.Sr-Nd-Pb Isotopic Characteristics of Ore-Bearing Host Rocks in Hongshiquan Uranium Deposit, Gansu. Acta Mineralogica Sinica, 35(Suppl.):175-176(in Chinese).
[43] Yang, W.T., Duan, L.Z., Zhang, Y., 2013. Studying in Middle-Tectonic Level and Rock Deformation Characteristic in Longshoushan Area. Northwestern Geology, 46(2): 44-53(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xbdz201302006
[44] Zhai, M. G., 2011. Cratonization and the Ancient North China Continent: A Summary and Review. Science China Earth Sciences, 41(8): 1037-1046(in Chinese). http://cn.bing.com/academic/profile?id=79b3f2b0efdb7e7af14fe8292e5588f5&encoded=0&v=paper_preview&mkt=zh-cn
[45] Zhang, C., 1989.Diagenetic Characteristics and Geological Implications of Granite-Grained Granite in Hongshuquan Uranium Deposit. Northwestern Geology, 22(1): 28-34(in Chinese).
[46] Zhang, W.L., Zou, M.Q., Shao, F., et al., 2009. Geological Characteristics of Dike-Structural Belt in Taoshan Orefield and Its Relationship to Uranium Deposits. World Nuclear Geoscience, 26(1): 38-42, 48(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=sjhdzkx200901006
[47] Zhang, Z.M., Ding, H.X., Dong, X., et al., 2018. High-Temperature Metamorphism, Anataxis and Tectonic Evolution of a Mafic Granulite from the Eastern Himalayan Orogen. Journal of Earth Science, 29(5): 1005-1009. https://doi.org/10.1007/s12583-018-0852-y
[48] Zhao, J.G., Wang, L.C., 2009. Discussion on Characteristics and Genesis Type of Hongshiquan Uranium Deposit. Gold Science and Technology, 17(1): 38-41(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hjkxjs200901009
[49] Zhao, Z.X., Jia, Y.Q., Wang, J.R., et al., 2018.LA-ICP-MS Zircon U-Pb Age and Geochemistry of Monzonite Granite-Quartz Diorite Pluton in Xiaoheishan Area of Beishan Orogenic Belt and Its Geological Significance, Inner Mongolia.Earth Science, 43(Suppl.2):49-59(in Chinese with English abstract).
[50] Zhou, D.W., Zhang, C.L., Liu, L., et al., 1998. Sm-Nd Dating of Basic Dykes from Wudang Block and a Discussion of Related Questions. Acta Geoscientia Sinica, 19(1): 25-30(in Chinese with English abstract).
[51] Zhou, Z.L., 1987.Characteristics and Genesis of the Cenozoic Lamprophyre Reservoir in Chezhen Depression. Bulletin of Mineralogy, Petrology and Geochemistry, 6(2): 66-68(in Chinese).
[52] 陈能松, 王新宇, 张宏飞, 等, 2007.柴-欧微地块花岗岩地球化学和Nd-Sr-Pb同位素组成:基底性质和构造属性启示.地球科学, 32(1):7-21. doi: 10.3321/j.issn:1000-2383.2007.01.002
[53] 陈文, 万渝生, 李华芹, 等, 2011.同位素地质年龄测定技术及应用.地质学报, 85(11):1917-1947. http://d.old.wanfangdata.com.cn/Periodical/dizhixb201111009
[54] 陈宣谕, 李红中, 卢文姬, 等, 2011.煌斑岩相关研究进展综述.中山大学研究生学刊(自然科学·医学版), 32(4):21-29. http://d.old.wanfangdata.com.cn/Periodical/dtsj201728051
[55] 陈毓川, 常印佛, 裴荣富, 等, 2007.中国成矿体系与区域成矿评价.北京:地质出版社.
[56] 管涛, 黄智龙, 谢力华, 等, 2003.云南白马寨镍矿区煌斑岩地球化学Ⅰ.主要元素和微量元素.矿物学报, 23(3):278-288. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kwxb200303016
[57] 侯贵廷, 2012.华北基性岩墙群.北京:科学出版社.
[58] 胡瑞忠, 金景福, 1990.贵东花岗岩体中煌斑岩的成因.矿物岩石, 10(4):1-7. http://www.cqvip.com/Main/Detail.aspx?id=315222
[59] 黄智龙, 刘丛强, 朱成明, 等, 1999.云南老王寨金矿区煌斑岩成因及其与金矿化的关系.北京:地质出版社.
[60] 李昌年, 1992.构造岩浆判别的地球化学方法及其讨论.地质科技情报, 11(3):73-78, 84. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000000361809
[61] 李世超, 张凌宇, 李鹏川, 等, 2017.大兴安岭中段早三叠世O型埃达克岩的发现及其大地构造意义.地球科学, 42(12):2117-2128. http://d.old.wanfangdata.com.cn/Periodical/dqkx201712002
[62] 黎彤, 倪守斌, 1997.中国大陆岩石圈的化学元素丰度.地质与勘探, 33(1):31-37. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199701016715
[63] 李献华, 周汉文, 韦刚健, 等, 2002.滇西新生代超钾质煌斑岩的元素和Sr-Nd同位素特征及其对岩石圈地幔组成的制约.地球化学, 31(1):26-34. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqhx200201005
[64] 李永军, 李甘雨, 佟丽莉, 等, 2015.玄武岩类形成的大地构造环境Ta、Hf、Th、La、Zr、Nb比值对比判别.地球科学与环境学报, 37(3):14-21. doi: 10.3969/j.issn.1672-6561.2015.03.004
[65] 凌洪飞, 徐士进, 沈渭洲, 等, 1998.格宗、东谷岩体Nd、Sr、Pb、O同位素特征及其与扬子板块边缘其它晋宁期花岗岩对比.岩石学报, 14(3):269-277. http://d.old.wanfangdata.com.cn/Periodical/ysxb98199803001
[66] 刘燊, 胡瑞忠, 冯光英, 等, 2010.华北克拉通中生代以来基性岩墙群的分布及研究意义.地质通报, 29(2-3):259-267. http://d.old.wanfangdata.com.cn/Periodical/zgqydz201002010
[67] 刘治恒, 巫晓兵, 2009.中基性脉岩与铀成矿的关系.现代矿业, 25(3):77-80. doi: 10.3969/j.issn.1674-6082.2009.03.022
[68] 卢磊勋, 杜萌, 邵瀚石, 2015. K-Ar法和Ar-Ar法两种定年方法的差异性对比及讨论.辽宁化工, 44(8):1025-1027. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=lnhg201508041
[69] 路凤香, 舒小辛, 赵崇贺, 1991.有关煌斑岩分类的建议.地质科技情报, 10(S1):55-62. http://www.cnki.com.cn/Article/CJFDTotal-DZKQ1991S1006.htm
[70] 马永非, 刘永江, 温泉波, 等, 2017.大兴安岭中段晚三叠世哈达陶勒盖组火山岩成因及构造背景.地球科学, 42(12):2146-2173. http://d.old.wanfangdata.com.cn/Periodical/dqkx201712004
[71] 戎嘉树, 韩泽宏, 夏毓亮, 1984.我国一岩体型铀矿床的矿化特征及成矿作用.放射性地质, 2(2):1-11. http://www.cnki.com.cn/Article/CJFDTotal-YKDZ198402000.htm
[72] 孙景贵, 胡受奚, 凌洪飞, 等, 2000.胶西北两类金矿田的高钾-钾质脉岩元素地球化学与成岩作用研究.地球化学, 29(2):143-152. doi: 10.3321/j.issn:0379-1726.2000.02.006
[73] 孙悦, 李巨初, 丁俊, 等, 2017.冕西煌斑岩脉型铀矿化特征及成因.四川地质学报, 37(2):209-213. doi: 10.3969/j.issn.1006-0995.2017.02.008
[74] 宋新宇, 覃功炯, 1994, 煌斑岩的成矿意义.矿产与地质, 8(2):81-87. http://d.old.wanfangdata.com.cn/Periodical/scyj201706009
[75] 瓦西拉里, 李红中, 梁锦, 等, 2011.煌斑岩的种类、成因及其与成矿作用的关系.中山大学研究生学刊(自然科学.医学版), 32(4):1-13. http://www.cnki.com.cn/Article/CJFDTotal-YJSK201104003.htm
[76] 王正其, 李子颖, 张国玉, 等, 2007.下庄中洞地区白垩纪基性脉岩地球化学特征及其源区性质.铀矿地质, 23(4):218-225, 248. doi: 10.3969/j.issn.1000-0658.2007.04.005
[77] 肖成东, 张忠良, 赵利青, 2004.东蒙地区燕山期花岗岩Nd、Sr、Pb同位素及其岩石成因.中国地质, 31(1):57-63. http://d.old.wanfangdata.com.cn/Periodical/zgdizhi200401008
[78] 辛存林, 马维云, 安国堡, 等, 2013.甘肃龙首山207铀矿床成矿地质特征及其成矿机制探讨.地质学报, 87(4):577-590. http://d.old.wanfangdata.com.cn/Periodical/dizhixb201304011
[79] 许德如, 2000.海南岛戈枕含金剪切带煌斑岩与金成矿关系研究.大地构造与成矿学, 24(3):258-265. doi: 10.3969/j.issn.1001-1552.2000.03.010
[80] 许继锋, 邱家骧, 1991.山东临朐山旺地区玄武岩浆的分离结晶.地球科学, 16(4):369-376. http://www.cnki.com.cn/Article/CJFDTotal-DQKX199104003.htm
[81] 杨春四, 张树明, 赵亚云, 等, 2015.甘肃红石泉铀矿床含矿主岩Sr-Nd-Pb同位素特征及意义.矿物学报, 35(S1):175-176. http://d.old.wanfangdata.com.cn/Conference/9132894
[82] 杨望暾, 段立志, 张阳, 2013.龙首山地区中深构造层次及岩石变形特征研究.西北地质, 46(2):44-53. doi: 10.3969/j.issn.1009-6248.2013.02.006
[83] 翟明国, 2011.克拉通化与华北陆块的形成.中国科学:地球科学, 41(8):1037-1046. http://www.cnki.com.cn/Article/CJFDTotal-JDXK201108001.htm
[84] 张诚, 1989.红石泉铀矿床含矿伟晶状白岗岩成岩特征及其地质意义.西北地质, 22(1):28-34. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000003277011
[85] 张万良, 邹茂卿, 邵飞, 等, 2009.桃山矿田脉岩-构造带地质特征及其与铀成矿的关系.世界核地质科学, 26(1):38-42, 48. doi: 10.3969/j.issn.1672-0636.2009.01.006
[86] 赵建国, 王龙成, 2009.红石泉铀矿床矿化特征及成因类型探讨.黄金科学技术, 17(1):38-41. doi: 10.3969/j.issn.1005-2518.2009.01.009
[87] 赵志雄, 贾元琴, 王金荣, 等, 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.地球科学, 43(S2):49-59. http://www.cnki.com.cn/Article/CJFDTotal-DQKX2018S2005.htm
[88] 周鼎武, 张成立, 刘良, 等, 1998.武当地块基性岩墙群的Sm-Nd定年及其相关问题讨论.地球学报, (1):25-30. http://www.cnki.com.cn/Article/CJFDTotal-DQXB801.003.htm
[89] 周自立, 1987.车镇凹陷中生代煌斑岩储油层的特征及成因.矿物岩石地球化学通讯, 6(2):66-68. http://www.cnki.com.cn/Article/CJFDTotal-KYDH198702007.htm