[1] Amelin, Y., Lee, D.C., Halliday, A.N., 2000. Early-Middle Archaean Crustal Evolution Deduced from Lu-Hf and U-Pb Isotopic Studies of Single Zircon Grains. Geochimica et Cosmochimica Acta, 64(24):4205-4225. https://doi.org/10.1016/S0016-7037(00)00493-2 http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=9483bc569d4dfe9bebecf8aee168fcb9
[2] Chappell, B. W., White, A. J. R., Williams, I. S., et al., 2004. Low- and High-Temperature Granites. Transactions of the Royal Society of Edinburgh Earth Sciences, 95(1-2):125-140. https://doi.org/10.1017/S0263593300000973
[3] Chen, G.Z., Wu, G., Li, T.G., et al., 2018. LA-ICP-MS Zircon and Cassiterite U-Pb Ages of Daolundaba Copper-Tungstentin Deposit in Inner Mongolia and Their Geological Significance. Mineral Deposits, 37(2):225-245(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kcdz201802002
[4] Cheng, Y., Xiao, Q.H., Li, T.D., et al., 2019. Magmatism and Tectonic Background of Early Permian Intra-Oceanic Arc in Diyanmiao Subduction Accretion Complex Belt in Eastern Margin of Central Asian Orogenic Belt. Earth Science, 44(10):3454-3468(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201910018
[5] Duan, M., Zeng, W., Feng, X.X., et al., 2016. LA-ICP-MS Zircon U-Pb Ages and Geological Features of Daolundaba Granite in Xilinhaote Area, Inner Mongolia. Geological Bulletin of China, 35(7):1207-1216(in Chinese with English abstract). http://www.researchgate.net/publication/306167591_LA-ICP-MS_zircon_U-Pb_ages_and_geological_features_of_Daolundaba_granite_in_Xilinhaote_area_Inner_Mongolia
[6] Dubińska, E., Bylina, P., Kozłowski, A., et al., 2004. U-Pb Dating of Serpentinization:Hydrothermal Zircon from a Metasomatic Rodingite Shell (Sudetic Ophiolite, SW Poland). Chemical Geology, 203(3/4):183-203. https://doi.org/10.1016/j.chemgeo.2003.10.005
[7] Elhlou, S., Belousova, E., Griffin, W. L., et al., 2006. Trace Element and Isotopic Composition of GJ-Red Zircon Standard by Laser Ablation. Geochimica et Cosmochimica Acta, 70(18):A158. https://doi.org/10.1016/j.gca.2006.06.1383 http://adsabs.harvard.edu/abs/2006GeCAS..70R.158E
[8] Fan, Y.X., Li, T.D., Xiao, Q.H., et al., 2019. Zircon U-Pb Ages, Geochemical Characteristics of Late Permian Granite in West Ujimqin Banner, Inner Mongolia, and Tectonic Significance.Geological Review, 65(01):248-266(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlp201901022
[9] Feng, J. R., Zhou, Z. H., Che, H. W., 2017. Permian Copper-Polymetallic Mineralization in the Southern Great Xing'an Range, Northeast China:The Daolundaba Copper-Polymetallic Deposit Example. International Geology Review, 59(13):1709-1722. doi: 10.1080/00206814.2017.1294508
[10] Ferry, J. M., Watson, E. B., 2007. New Thermodynamic Models and Revised Calibrations for the Ti-in-Zircon and Zr-in-Rutile Thermometers. Contributions to Mineralogy and Petrology, 154(4):429-437. https://doi.org/10.1007/s00410-007-0201-0 http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=90415b9781bec3f04a9c708eaaae3c6e
[11] Gao, S., Liu, X. M., Yuan, H. L., et al., 2002. Determination of Forty Two Major and Trace Elements in USGS and NIST SRM Glasses by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry. Geostandards and Geoanalytical Research, 26(2):181-196. https://doi.org/10.1111/j.1751-908x.2002.tb00886.x
[12] Gao, X. F., Guo, F., Xiao, P. X., et al., 2016. Geochemical and Sr-Nd-Pb Isotopic Evidence for Ancient Lower Continental Crust beneath the Xi Ujimqin Area of NE China. Lithos, 252-253:173-184. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=5e75a928af4e492893f5527a53dc88db
[13] Grimes, C. B., John, B. E., Kelemen, P. B., et al., 2007. Trace Element Chemistry of Zircons from Oceanic Crust:A Method for Distinguishing Detrital Zircon Provenance. Geology, 35(7):643. https://doi.org/10.1130/g23603a.1
[14] Hoskin, P. W. O., 2005. Trace-Element Composition of Hydrothermal Zircon and the Alteration of Hadean Zircon from the Jack Hills, Australia. Geochimica et Cosmochimica Acta, 69(3):637-648. https://doi.org/10.1016/j.gca.2004.07.006 http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=49d8b1f94427b2601dc76aff1be60760
[15] Jiang, S.H., Nei, F.J., Bai, D.M., et al., 2011. Geochronology Evidence for Indosinian Mineralization in Baiyinnuoer Pb-Zn Deposit of Inner Mongolia. Mineral Deposits, 30(5):787-798(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kcdz201105003
[16] Jiang, S.H., Zhang, L.L., Liu, Y.F., et al., 2018. Metallogeny of Xing-Meng Orogenic Belt and Some Related Problems. Mineral Deposits, 37(4):671-711(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kcdz201804001
[17] Li, G.Z., Wang, Y.J., Li, C.Y., et al., 2017. Discovery of Early Permian Radiolarian Fauna in the Solon Obo Ophiolite Belt, Inner Mongolia and Its Geological Significance. Chinese Science Bulletin, 62(5):400-406.https://https://doi.org/10.1360/N972016-00703. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kxtb201705007
[18] Li, T.D., Xiao, Q.H., Pan, G.T., et al., 2019. A Consideration about the Development of Ocean Plate Geology. Earth Science, 44(5):1441-1451(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201905003
[19] Li, S.Q., Chen, Y.J., Han, R.D., et al., 2017. Chronology and Geochemistry of Meta-Basic Volcanics of Baiyinnuoer Region in Wenduermiao Area, Inner Mongolia. Global Geology, 36(2):428-440(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=sjdz201702010
[20] Liu, J.F., Li, J.Y., Sun, L.X., et al., 2016. Zircon U-Pb Dating of the Jiujingzi Ophiolite in Bairin Left Banner, Inner Mongolia:Constraints on the Formation and Evolution of the Xar Moron River Suture Zone. Geology in China, 43(6):1947-1962(in Chinese with English abstract). doi: 10.12029/gc20160607
[21] Liu, R.L., Wu, G., Li, T.G., et al., 2018. LA-ICP-MS Cassiterite and Zircon U-Pb Ages of the Weilasituo Tin-Polymetallic Deposit in the Southern Great Xing'an Range and Their Geological Significance. Earth Science Frontiers, 25(5):183-201(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201805012
[22] Miller, C. F., McDowell, S. M., Mapes, R. W., 2003. Hot and Cold Granites? Implications of Zircon Saturation Temperatures and Preservation of Inheritance. Geology, 31(6):529. https://doi.org/10.1130/0091-7613(2003)031<0529:hacgio>2.0.co;2 doi: 10.1130/0091-7613(2003)031<0529:hacgio>2.0.co;2
[23] Pan, G.T., Xiao, Q.H., Zhang, K.X., et al., 2019. Recognition of the Oceanic Subduction-Accretion Zones from the Orogenic Belt in Continents and Its Important Scientific Significance. Earth Science, 44(5):1544-1561(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201905012
[24] Pan, X.F., Wang, S., Hou, Z.Q., et al., 2009. Geology and Metallogenesis of Daolundaba Copper Polymetallic Deposits, Inner Mongolia. Mineralogica, 33(3):402-410(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ddgzyckx200903011
[25] Shao, J.A., Tian, W., Tang, K., D., et al., 2018. Preliminary Discussion on the Role of Microcontinental Blocks in the Evolution of the Central Asian orogenic belt:Taking the Xilinhaote Microcontinental Block as an Example. Earth Science Frontiers, 25(4):1-10(in Chinese with English abstract).
[26] Shao, J.A., Zhang, L.Q., Mou, B. L., 1998. The Mesozoic Tectono-Thermal Evolution in the Middle and South of Daxing'Anling. Science in China(Series D:Earth Sciences), (3):193-200(in Chinese with English abstract).
[27] 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
[28] Tao, J.X., Hu, F.X., Chen, Z.Y., 2003. Characteristics and Tectonic Environment of S-Type Granite Belt in the Northern Margin of the North China Block. Acta Petrologica et Mineralogica, (2):112-118.(in Chinese with English abstract)
[29] Vervoort, J. D., Patchett, P. J., Gehrels, G. E., et al., 1996. Constraints on Early Earth Differentiation from Hafnium and Neodymium Isotopes. Nature, 379(6566):624-627. https://doi.org/10.1038/379624a0
[30] Wang, W.J., Sun, Z.J., Hu, X.Z., 2005. Geological Characters and Tectonic Setting of Qianjinchang Granite in Inner Mongolia. Geology and Prospecting, 41(2):35-40(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzykt200502008
[31] Wang, Q., Zhu, D. C., Zhao, Z. D., et al., 2012. Magmatic Zircons from I-, S- and A-Type Granitoids in Tibet:Trace Element Characteristics and Their Application to Detrital Zircon Provenance Study. Journal of Asian Earth Sciences, 53:59-66. https://doi.org/10.1016/j.jseaes.2011.07.027
[32] Watson, E.B., Harrison, H.T., 2005. Zircon Thermometer Reveals Minimum Melting Conditions on Earliest Earth. Science, 308(5723):841-844.https://10.1126/science.1110873 http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=a5e61c2f3bbfcdb60fc5fb695bffa13f
[33] Wu, F.Y., Li, X.H., Yang, J.H., et al., 2007a. Discussions on the Petrogenesis of Granites. Acta Petrologica Sinica, 23(6):1217-1238(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200706001
[34] Wu, F.Y., Li, X.H., Zheng, Y.F., et al., 2007b. Lu-Hf Isotopic Systematics and Their Applications in Petrology. Acta Petrologica Sinica, 23(2):185-220(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200702001
[35] Xiao, Q.H., Li, T.D., Pan, G.T., et al., 2016. Petrologic Ideas for Identification of Ocean-Continent Transition:Recognition of Intra-Oceanic Arc and Initial Subduction. Geology in China, 43(3):721-737(in Chinese with English abstract). doi: 10.12029/gc20160303
[36] Xiao, W.J., Brian, W., Jie, F.H., et al., 2003. Accretion Leading to Collision and the Permian Solonker Suture, Inner Mongolia, China:Termination of the Central Asian Orogenic Belt.Tectonics, 22(6). https://doi.org/10.1029/2002tc001484
[37] Xu, B., Zhao, P., Bao, Q.Z., et al., 2014. Preliminary Study on the Pre-Mesozoic tectonic Unit Division of the Xing-Meng Orogenic Belt (XMOB). Acta Petrologica Sinica, 30(7):1841-1857(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201407001
[38] Xu, J.J., Lai, Y., Cu, D., et al., 2009. Characteristics and Evolution of Ore-Forming Fluids of the Daolundaba Copper-Poly-Metal Deposit, Inner Mongolia. Acta Petrologica Sinica, 25(11):2957-2972(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200911025
[39] Yao, M.J., Cao, Y., Lui, J.J., et al., 2016. Isotope Age of Re-Os in Molybdenite and Genetic Implication of Huanggangliang Fe-Sn Deposit in Inner Mongolia. Mineral Exploration, 7(3):399-403(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ytgcj201603003
[40] Zhai, D.G., Lui, J.J., Yang, Y.Q., et al., 2012. Petrogenetic and Metallogentic Ages and Tectonic Setting of the Huanggangliang Fe-Sn Deposit, Inner Mongolia. Acta Petrologica et Mineralogica, 31(4):513-523(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yskwxzz201204004
[41] Zhang, T.F., Guo, S., Xin, H.T., et al., 2019. Petrogenesis and Magmatic Evolution of Highly Fractionated Granite and Their Constraints on Sn-(Li-Rb-Nb-Ta) Mineralization in the Weilasituo Deposit, Inner Mongolia, Southern Great Xing'an Range, China. Earth Science, 44(1):248-267(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201901018
[42] Zhao, Y.L., Li, W.M., Wen, Q.B., et al., 2016. Late Paleozoic Tectonic Framework of Eastern Inner Mongolia:Evidence from the Detrital Zircon U-Pb Ages of the Mid-Late Permian to Early Triassic sandstones. Acta Petrologica Sinica, 32(9):807-2822(in Chinese with English abstract).
[43] Zhao, Z.H., 2010. Trace Element Geochemistry of Accessory Minerals and iIts Applications in Petrogenesis and Metallogenesis. Earth Science Frontiers, 17(1):267-286(in Chinese with English abstract). http://www.researchgate.net/publication/280982588_Trace_element_geochemistry_of_accessory_minerals_and_its_applications_in_petrogenesis_and_metallogenesis
[44] Zhou, A.R.G.L., Dai, J.G., Li, Y.L., et al., 2017. Zircon Trace Element Geochemical Characteristics of Late Silurian-Early Jurassic Granitoids from Eastern Kunlun Range and Its Geological Significance. Acta Petrologica Sinica, 33(1):173-190. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201701015
[45] Zhou, Z.H., Lv, L.S., Feng, J.R., et al., 2010. Molybdenite Re-Os Ages of Huanggang Skarn Sn-Fe Deposit and their Geological Significance, Inner Mongolia. Acta Petrologica Sinica, 26(3):667-679(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201003003
[46] Zhou, Z.H., Lv, L.S., Yang, Y.J., et al., 2010. Petrogenesis of the Early Cretaceous A-Type Granite in the Huanggang Sn-Fe Deposit, Inner Mongolia:Constraints from Zircon U-Pb Dating and Geochemistry. Acta Petrologica Sinica, 26(12):3521-3537(in Chinese with English abstract). doi: 10.1071/BT9710085
[47] Zhou, Z.H., Ouyang, H.G., Wu, X.L., et al., 2014. Geochronology and Geochemistry Study of the Biotite Granite from the Daolundaba Cu-W Polymetallic Deposit in the Inner Mogolia and Its Geological Significance. Acta Petrologica Sinica, 30(1):79-94(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201401006
[48] 陈公正, 武广, 李铁刚, 等, 2018.内蒙古道伦达坝铜钨锡矿床LA-ICP-MS锆石和锡石U-Pb年龄及其地质意义.矿床地质, 37(2):30-50. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kcdz201802002
[49] 程杨, 肖庆辉, 李廷栋, 等, 2019.中亚造山带东缘迪彦庙俯冲增生杂岩带早二叠世洋内弧岩浆作用及构造背景.地球科学, 44(10):3454-3468. doi: 10.3799/dqkx.2019.085
[50] 段明, 曾威, 冯晓曦, 等, 2016.内蒙古锡林浩特地区道伦达坝矿区花岗岩LA-ICP-MS锆石U-Pb年龄及其地质意义.地质通报, (7):1207-1216. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz201607015
[51] 范玉须, 李廷栋, 肖庆辉, 等, 2019.内蒙古西乌珠穆沁旗晚二叠世花岗岩的锆石U-Pb年龄、地球化学特征及其构造意义.地质论评, 65(1):248-266. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlp201901022
[52] 江思宏, 聂凤军, 白大明, 等, 2011.内蒙古白音诺尔铅锌矿床印支期成矿的年代学证据.矿床地质, 30(5):787-798. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kcdz201105003
[53] 江思宏, 张莉莉, 刘翼飞, 等, 2018.兴蒙造山带成矿规律及若干科学问题.矿床地质, 37(4):671-711. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kcdz201804001
[54] 李钢柱, 王玉净, 李成元, 等, 2017.内蒙古索伦山蛇绿岩带早二叠世放射虫动物群的发现及其地质意义.科学通报, (5):60-66. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kxtb201705007
[55] 李尚启, 陈跃军, 韩仁道, 等, 2017.内蒙古温都尔庙地区白音诺尔一带变质基性火山岩年代学和地球化学研究.世界地质, 36(2):428-440. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=sjdz201702010
[56] 李廷栋, 肖庆辉, 潘桂棠, 等, 2019.关于发展洋板块地质学的思考.地球科学, 44(5):1441-1451. doi: 10.3799/dqkx.2019.970
[57] 刘建峰, 李锦轶, 孙立新, 等, 2016.内蒙古巴林左旗九井子蛇绿岩锆石U-Pb定年:对西拉木伦河缝合带形成演化的约束.中国地质, 43(6):1947-1962. http://www.cqvip.com/QK/90050X/201606/7000084551.html
[58] 刘瑞麟, 武广, 李铁刚, 等, 2018.大兴安岭南段维拉斯托锡多金属矿床LA-ICP-MS锡石和锆石U-Pb年龄及其地质意义.地学前缘, 25(5):183-201. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201805012
[59] 潘桂棠, 肖庆辉, 张克信, 等, 2019.大陆中洋壳俯冲增生杂岩带特征与识别的重大科学意义.地球科学, 44(5):1545-1561. doi: 10.3799/dqkx.2019.063
[60] 潘小菲, 王硕, 侯增谦, 等, 2009.内蒙古道伦达坝铜多金属矿床特征研究.大地构造与成矿学, 33(03):402-410. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ddgzyckx200903011
[61] 邵济安, 田伟, 唐克东, 等, 2018.初论微陆块在中亚造山带演化中的作用:以锡林浩特微陆块为例.地学前缘, 25(4):1-10. http://d.old.wanfangdata.com.cn/Periodical/dxqy201804001
[62] 邵济安, 张履桥, 牟保磊, 1998.大兴安岭中南段中生代的构造热演化.中国科学(D辑:地球科学), (3):2-9 http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199800269868
[63] 陶继雄, 胡凤翔, 陈志勇, 2003.华北陆块北缘印支期S型花岗岩带特征及其构造环境.岩石矿物学杂志, (2):112-118. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yskwxzz200302002
[64] 王万军, 孙振家, 胡祥昭, 2005.内蒙古前进场花岗岩体的地质特征及其构造环境.地质与勘探, 41(2):35-40. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzykt200502008
[65] 吴福元, 李献华, 杨进辉, 等, 2007a.花岗岩成因研究的若干问题.岩石学报, 23(6):3-24. doi: 10.3969/j.issn.1000-0569.2007.06.001
[66] 吴福元, 李献华, 郑永飞, 等, 2007b. Lu-Hf同位素体系及其岩石学应用.岩石学报, 23(2):185-220. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200702001
[67] 肖庆辉, 李廷栋, 潘桂棠, 等, 2016.识别洋陆转换的岩石学思路——洋内弧与初始俯冲的识别.中国地质, 43(3):721-737. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi201603003
[68] 徐备, 赵盼, 鲍庆中, 等, 2014.兴蒙造山带前中生代构造单元划分初探.岩石学报, 30(7):1841-1857. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201407001
[69] 徐佳佳, 赖勇, 崔栋, 等, 2009.内蒙古道伦达坝铜多金属矿床成矿流体特征及其演化.岩石学报, (11):2957-2972. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200911025
[70] 要梅娟, 曹烨, 刘家军, 等, 2016.内蒙古黄岗梁铁锡矿床辉钼矿Re-Os年龄及其成因意义.矿产勘查, 7(3):399-403. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ytgcj201603003
[71] 翟德高, 刘家军, 杨永强, 等, 2012.内蒙古黄岗梁铁锡矿床成岩、成矿时代与构造背景.岩石矿物学杂志, 31(4):513-523. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yskwxzz201204004
[72] 张天福, 郭硕, 辛后田, 等, 2019.大兴安岭南段维拉斯托高分异花岗岩体的成因与演化及其对Sn-(Li-Rb-Nb-Ta)多金属成矿作用的制约.地球科学, 44(1):248-267. doi: 10.3799/dqkx.2018.246
[73] 赵英利, 李伟民, 温泉波, 等, 2016.内蒙东部晚古生代构造格局:来自中、晚二叠-早三叠世砂岩碎屑锆石U-Pb年代学的证据.岩石学报, 32(9):2807-2822. http://www.cnki.com.cn/Article/CJFDTotal-YSXB201609015.htm
[74] 赵振华, 2010.副矿物微量元素地球化学特征在成岩成矿作用研究中的应用.地学前缘, (1):269-288. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201001022
[75] 周敖日格勒, 戴紧根, 李亚林, 等, 2017.东昆仑山脉晚志留世-早侏罗世花岗类岩石中锆石微量元素地球化学特征及地质意义.岩石学报, (1):173-189. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201701015
[76] 周振华, 吕林素, 冯佳睿, 等, 2010.内蒙古黄岗夕卡岩型锡铁矿床辉钼矿Re-Os年龄及其地质意义.岩石学报, 26(3):667-679. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201003003
[77] 周振华, 吕林素, 杨永军, 等, 2010.内蒙古黄岗锡铁矿区早白垩世A型花岗岩成因:锆石U-Pb年代学和岩石地球化学制约.岩石学报, 26(12):3521-3537. http://www.cnki.com.cn/Article/CJFDTotal-YSXB201012007.htm
[78] 周振华, 欧阳荷根, 武新丽, 等, 2014.内蒙古道伦达坝铜钨多金属矿黑云母花岗岩年代学、地球化学特征及其地质意义.岩石学报, 30(1):79-94. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201401006