Re-Os Isotopic Ages of Two Types of Molybdenite from Zhangdongkeng Tungsten Deposit in Southern Jiangxi Province and Their Geologic Implications
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摘要: 赣南樟东坑钨矿具有典型的"上脉(黑钨矿石英脉)下体(蚀变细粒花岗岩)"和"上钨下钼"矿化模式, 为了弄清黑钨矿石英脉与蚀变细粒岩体型矿化之间在成矿时间上的关系, 对产于该矿细粒花岗岩中的辉钼矿和石英脉中的辉钼矿分别进行了Re-Os同位素定年. 测试结果为: 细粒花岗岩中的3件辉钼矿样品Re-Os等时线年龄为155.4±2.1 Ma(MSWD=1.12), 模式年龄154.9±2.6 Ma~156.5 ± 2.6 Ma, 加权平均年龄155.5±1.4 Ma(MSWD=0.44);而石英脉中5件辉钼矿样品的Re-Os等时线年龄为154.6±1.7 Ma(MSWD=0.030), 模式年龄变化范围为154.2±2.3 Ma~154.7±2.7 Ma, 加权平均年龄为154.29±0.98 Ma(MSWD=0.045). 上述结果表明, 花岗岩体型矿化与石英脉型矿化的年龄在误差范围内高度一致, 从而证明了岩体中的钼钨矿化与石英脉中的钨钼矿化为同一次岩浆热液矿化事件的产物.Abstract: Zhangdongkeng tungsten deposit has a special mineralization model, which is a quartz vein type mineralization in the upper portion while an altered granite type mineralization in the lower part. It also shows that tungsten was enriched in the upper part while molybdenum enriched in the lower. Molybdenites in fine-grained granite and quartz vein were separately used for Re-Os dating to test the temporal relation of the two types of mineralization. The isochron age of three molybdenite samples in fine-grained granite is 155.4±2.1 Ma (MSWD=1.12), with model ages of them between 154.9±2.6 Ma and 156.5±2.6 Ma, and the weighted average age 155.5±1.4 Ma (MSWD=0.44). Five molybdenite samples in quartz vein yield a Re-Os isochron age of 154.6±1.7 Ma (MSWD=0.030), with model ages 154.2±2.3 Ma to 154.7±2.7 Ma, and the weighted mean age is 154.29±0.98 Ma (MSWD=0.045). The results show that the ages of altered granite type mineralization and quartz vein type mineralization are basically almost same, which well indicates that molybdenites in both mineralization types are products of the same magmatic-hydrothermal event.
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图 2 樟东坑钨矿区地质略图
1.中寒武统高滩群；2.破碎带；3.石英脉；4.背向斜轴线；5.剖面；6.石英脉组编号；7.蚀变花岗岩型钼钨矿体；8.细粒花岗岩
Fig. 2. Simplified geological map of Zhangdongkeng tungsten deposit area
图 3 樟东坑矿区I组钼矿化垂向分带示意(据幸世军等，2010)
1.地形线；2.钨矿化带下界；3.钨钼矿化带下界；4.钼钨矿化带下界；5.蚀变花岗岩型钼钨矿体；6.细粒花岗岩
Fig. 3. Vertical zoning Schematic diagram of molybdenum mineralization in Zhangdongkeng veins of group I
图 4 两种钼矿化野外典型照片
a~c.石英脉型钼矿化；d~f.花岗岩脉侧钼矿化
Fig. 4. Representative photos of two types of molybdenum mineralization
图 5 樟东坑钨矿两种辉钼矿Re-Os同位素等时线年龄及模式年龄加权平均值
a.石英脉型矿化中辉钼矿Re-Os等时线年龄；b.石英脉型矿化中辉钼矿Re-Os模式年龄加权平均值；c.岩体型矿化中辉钼矿Re-Os等时线年龄；d.岩体型矿化中辉钼矿Re-Os模式年龄加权平均值
Fig. 5. Re-Os isochron of molybdenites and weighted average of model ages of two types molybdenites from Zhangdongkeng deposit
表 1 樟东坑钨矿两种不同产状辉钼矿Re-Os同位素测试结果
Table 1. Data of Re-Os isotope analysis of two type molybdenites from Zhangdongkeng deposit
原样名 样重(g) Re (μg·g-1) 普Os(ng·g-1) 187Re (μg·g-1) 187Os (ng·g-1) 模式年龄(Ma) 测定值 不确定度 测定值 不确定度 测定值 不确定度 测定值 不确定度 测定值 不确定度 ZYN-6 0.405 11 0.578 0 0.005 9 0.000 2 0.001 0 0.363 3 0.003 7 0.948 5 0.009 5 156.5 2.6 ZYW-5 0.4005 3 0.307 0 0.002 8 0.000 2 0.000 2 0.192 9 0.001 7 0.499 6 0.005 4 155.2 2.5 ZYN-13 0.403 88 5.805 0 0.064 0 0.000 2 0.006 8 3.649 0 0.040 0 9.428 0 0.089 0 154.9 2.6 Zmn-2 0.400 46 0.212 2 0.001 7 0.043 4 0.000 9 0.133 4 0.001 1 0.343 1 0.003 3 154.2 2.3 Zmn-1 0.400 96 0.077 9 0.000 6 0.000 2 0.000 5 0.049 0 0.000 4 0.126 0 0.001 3 154.2 2.3 Zmn-3 0.400 78 0.098 1 0.000 8 0.000 2 0.000 2 0.061 7 0.000 5 0.158 6 0.001 3 154.2 2.2 Zmn-4 0.400 50 0.137 3 0.001 1 0.002 9 0.000 5 0.086 3 0.000 7 0.221 9 0.002 2 154.2 2.3 Zmn-5 0.401 10 0.526 6 0.004 1 0.001 7 0.000 7 0.331 0 0.002 6 0.854 1 0.006 7 154.7 2.1 
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Chen, G.W., Li, J., 1992. Characteristics of Deposit Occurrence and Statistical Analysis of Mining Losses in Zhangdongkeng Mine. Journal of Southern Institute of Metallurgy, 13(4): 271-278(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-NFYX199204000.htm Chen, R.S., Li, J.W., Cao, K., et al., 2013. Zircon U-Pb and Molybdenite Re-Os Dating of the Shangfang Tungsten Deposit in the Northern Fujian Province: Implications for Regional Mineralization. Earth Science—Journal of China University of Geosciences, 38(2): 289-304 (in Chinese with English abstract). doi: 10.3799/dqkx.2013.029 Chen, Z.H., Wang, D.H., Qu, W.J., et al., 2006. Geological Characteristics and Mineralization Age of the Taoxikeng Tungsten Deposit in Chongyi County, Southern Jiangxi Province, China. Geological Bulletin of China, 25(4): 496-501 (in Chinese with English abstract). http://www.researchgate.net/publication/280015317_Geological_characteristics_and_mineralization_age_of_the_Taoxikeng_tungsten_deposit_in_Chongyi_County_southern_Jiangxi_Province_China Du, A.D., Qu, W.J., Wang, D.H., et al., 2007. Subgrain-Size Decoupling of Re and 187Os within Molybdenite. Mineral Deposits, 26(5): 572-580 (in Chinese with English abstract). http://www.researchgate.net/publication/284889953_Subgrain-size_decoupling_of_Re_and_187Os_within_molybdenite Du, A.D., Wu, S.Q., Sun, D.Z., et al., 2004. Preparation and Certification of Re-Os Dating Reference Materials: Molybdenite HLP and JDC. Geostandard and Geoanalytical Research, 28(1): 41-52. doi: 10.1111/j.1751-908X.2004.tb01042.x Du, A.D., Zhao, D.M., Wang, S.X., et al., 2001. Precise Re-Os Dating for Molybdenite by IDNTIMS with Carius Tube Sample Preparation. Rock and Mineral Analysis, 20(4): 247-252(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YKCS200104001.htm Feng, C.Y., Feng, Y.D., Xu, J.X., et al., 2007a. Isotope Chronological Evidence for Upper Jurassic Petrogenesis and Mineralization of Altered Granite-Type Tungsten Deposits in the Zhangtiantang Area, Southern Jiangxi. Geology in China, 34(4): 642-650 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DIZI200704014.htm Feng, C.Y., Xu, J.X., Zeng, Z.L., et al., 2007b. Zircon SHRIMP U-Pb and Molybdenite Re-Os Dating in Tianmenshan-Hongtaoling Tungsten-Tin Orefield, Southern Jiangxi Province, China, and Its Geological Implication. Acta Geologica Sinica, 81(7): 952-963 (in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-dzxe200707010.htm Fu, J.M., Li, H.Q., Qu, W.J., et al., 2008. Determination of Mineralization Epoch of Quartz-Vein Type Tungsten Deposits in Shixing Region, Northern Guangdong and Its Geological Significance. Geotectonica et Metallogenia, 32(1): 57-62 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DGYK200801009.htm Gu, J.Y., 1981. Morphological Zoning of the Vein-Type Tungsten Deposits in South China. In: Yu, H.Z., ed., Proceeding of Symposium on Tungsten Geology. Geological Publishing House, Beijing, 35-45(in Chinese). He, L.T., 2003. Discussion on the Changing Rules of Mineral Veins and Inspecting Methods. China Tungsten Industry, 18(4): 15-19 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-ZGWU200304005.htm Hu, D.Q., Hua, R.M., Li, G.L., et al., 2011. Study on the Fluid Inclusions of Maoping Tungsten Deposit, Southern Jiangxi Province. Geological Journal of China Universities, 17(2): 327-336(in Chinese with English abstract). http://www.zhangqiaokeyan.com/academic-journal-cn_geological-journal-china-universities_thesis/0201253565586.html 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.researchgate.net/publication/284690423_Three_major_metallogenic_events_in_Mesozoic_in_South_China Hua, R.M., Zhang, W.L., Li, G.L., et al., 2008. A Preliminary Study on the Features and Geologic Implication of the Accompanying Metals in Tungsten Deposits in the Nanling Region. Geological Journal of China Universities, 14(4): 527-538 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GXDX200804008.htm Huang, X.E., Li, G.L., Guo, J.S., et al., 2012. Characteristics of Ore-Forming Granite and Its Mineralization in the Zhangdongkeng Tungsten Deposit of Southern Jiangxi Province. Geology and Exploration, 48(4): 685-692 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKT201204004.htm Li, B., 2011. Synchronization Theory and Tungsten-Polymetallic Mineralization Distribution in the Qianlishan-Qitianling Area, Southern Hunan. Journal of China University of Geosciences, 22(6): 726-736. doi: 10.1007/s12583-011-0223-4 Li, C., Qu, W.J., Du, A.D., 2009. Decoupling of Re and Os and Migration Model of 187Os in Coarse-Grained Molybdenite. Mineral Deposits, 28(5): 707-712(in Chinese with English abstract). http://d.wanfangdata.com.cn/periodical/kcdz200905016 Li, G.L., Hua, R.M., Huang, X. E, et. al., 2011a. Re-Os Isotopic Age of Molybdenite from the Xiatongling Tungsten Deposit, Central Jiangxi Province, and Its Geological Implications. Mineral Deposits, 30(6): 1075-1084(in Chinese with English abstract). Li, G.L., Hua, R.M., Wei, X. L, et al., 2011b. Rb-Sr Isochron Age of Single-Grain Muscovite in the Xushan W-Cu Deposit, Central Jiangxi, and Its Geological Significance. Earth Science—Journal of China University of Geosciences, 36(2): 282-288 (in Chinese with English abstract). Li, G.L., Hua, R.M., Zhang, W. L, 2011. He-Ar Isotope Composition of Pyrite and Wolframite in the Tieshanlong Tungsten Deposit, Jiangxi, China: Implications for Fluid Evolution. Resource Geology, 61(4): 356-366. doi: 10.1111/j.1751-3928.2011.00172.x Liu, J., Ye, H.S., Xie, G.Q., et al., 2008. Re-Os Dating of Molybdenite from the Hukeng Tungsten Deposit in the Wugongshan Area, Jiangxi Province, and Its Geological Implications. Acta Geologica Sinica, 82(11): 1576-1584 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE200811014.htm Liu, Y.J., Ma, D.S., 1987. Geochemistry of Tungsten. Science Press, Beijing (in Chinese). Ludwig, K.R., 2001. ISOPLOT/EX. Version 2.49, A Geochronological Toolkit for Microsoft Excel. Berkeley Geochronology Center, 1-20. Ma, D.S., 2009. Progress in Research on Geochemistry of Tungsten. Geological Journal of China Universities, 15(1): 19-34(in Chinese with English abstract). http://www.zhangqiaokeyan.com/academic-journal-cn_geological-journal-china-universities_thesis/0201253566003.html Mao, J.W., Zhang, Z.C., Zhang, Z.H., et al., 1999. Re-Os Isotopic Dating of Molybdenites in the Xiaoliugou W(Mo) Deposit in the Northern Qilian Mountains and Its Geological Significance. Geochimica et Cosmochimica Acta, 63(11-12): 1815-1818. doi: 10.1016/S0016-7037(99)00165-9 Qu, W.J., Du A.D., 2003. Highly Precise Re-Os Dating of Molybdenite by ICP-MS with Carius Tube Sample Digestion. Rock and Mineral Analysis, 22(4): 254-257 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YKCS200304003.htm Selby, D., Creaser, R.A., 2004. Macroscale NTIMS and Microscale LA-MC-ICP-MS Re-Os Isotopic Analysis of Molybdenite: Testing Spatial Rest Rictions for Reliable Re-Os Age Determinations, and Implications for the Decoupling of Re and Os with in Molybdenite. Geochimica et Cosmochimica Acta, 68(19): 3897-3908. doi: 10.1016/j.gca.2004.03.022 Shirey, S.B., Walker, R.J., 1995. Carius Tube Digestion for Low-Blank Rhenium-Osmium Analysis. Anal. Chem. , 67: 2136-2141. doi: 10.1021/ac00109a036 Smoliar, M.L., Walker, R.J., Morgan, J.W., 1996. Re-Os Ages of Group ⅡA, Ⅲa, ⅣA and ⅣB Iron Meteorites. Science, 271: 1099-1102. doi: 10.1126/science.271.5252.1099 Stein, H.J., Markey, R.J., Morgan, J.W., et al., 2001. The Remarkable Re-Os Chronometer in Molybdenite: How and Why It Works. Terra Nova, 13: 479-486. doi: 10.1046/j.1365-3121.2001.00395.x Tan, Y.J., 2000. An Opinion on the Second Round Exploration of Wolframite in Nanling Region. China Tungsten Industry, 15(6): 9-13(in Chinese with English abstract). Wang, D.H., Chen, Z.H., Chen, Y.C., et al., 2010. New Data of the Rock Forming and Ore-Forming Chronology for China's Important Mineral Resources. Acta Geologica Sinica, 84(7): 1030-1040(in Chinese with English abstract). http://www.researchgate.net/publication/284594588_New_data_of_the_rock-forming_and_ore-forming_chronology_for_China's_important_mineral_resources_areas Wang, X.F., Qi, H.W., Hu, R.Z., et al., 2010. Re-Os Isotopic Chronology of Molybdenites from Hongling Tungsten Deposit of Guangdong Province and Its Geological Significance. Mineral Deposits, 29(3): 415-426(in Chinese with English abstract). http://www.researchgate.net/publication/284485448_Re-Os_isotopic_chronology_of_molybdenites_from_Hongling_tungsten_deposit_of_Guangdong_Province_and_its_geological_significance Wei, X.L., 2001. Initiate New Prospect on the Geological Work of Tungsten Minerals. China Tungsten Industry, 16(5): 65-68(in Chinese with English abstract). http://www.ga.gov.au/data-pubs/data-and-publications-search/publications/aimr/tungsten Wei, X.L., 2012. The Metallogenic Features and Ore-Finding Potentiality of the Tungsten Deposits in South Jiangxi Province. China Tungsten Industry, 27(1): 14-21 (in Chinese with English abstract). http://www.researchgate.net/publication/285821188_The_metallogenic_features_and_ore-finding_potentiality_of_the_Tungsten_Deposits_in_South_Jiangxi_Province Wu, Y.L., Mei, Y.W., Liu, P.C., et al., 1987. Geology of the Xihuashan Tungsten Ore Field. Geological Publishing House, Beijing (in Chinese). Xia, H.Y., Liang, S.Y., 1986. Primary Zoning and Genetics Series of W, Sn(Ta, Nb) Ore Deposits in Nanling. Journal of Mineralogy and Petrology, 1: 1-182 (in Chinese with English abstract). Xing, S.J., Chen, D.S., Li, G.L., 2010. Analysis on the Vertical Distribution in the Zhangdongkeng W-Mo Deposit of Jiangxi. China Tungsten Industry, 25(5): 8-12 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZGWU201005005.htm Yang, Z.H., Wang, J.P., Liu, J, J., et al., 2012. Characteristics and Its Geological Significance of Fluid Incluisions of the Wurinitu W-Mo Deposit in Inner Mongolia, China. Earth Science—Journal of China University of Geosciences, 37(6): 1268-1278 (in Chinese with English abstract). http://www.researchgate.net/publication/288079622_Characteristics_and_its_geological_significance_of_fluid_inclusions_of_the_Wurinitu_W-Mo_Deposit_in_Inner_Mongolia_China Zeng, Z.L., Zhang, Y.Z., Zhu, X.P., et al., 2009. Re-Os Isotopic Dating of Molybdenite from the Maoping Tungsten-Tin Deposit in Chongyi County of Southern Jiangxi Province and Its Geological Significance. Rock and Mineral Analysis, 28(3): 209-214 (in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTotal-YKCS200903007.htm Zhang, J.J., Chen, Z.H., Wang, D.H., et al., 2008. Geological Characteristics and Metallogenic Epoch of the Xingluokeng Tungsten Deposit, Fujian Province. Geotectonica et Metallogenia, 32(1): 92-97 (in Chinese with English abstract). http://www.cqvip.com/Main/Detail.aspx?id=26509874 Zhang, W.L., Hua, R.M., Wang, R.C., et al., 2009. New Dating of the Piaotang Granite and Related Tungsten Mineralizationin, Southern Jiangxi. Acta Geologica Sinica, 83(5): 659-670 (in Chinese with English abstract). http://www.researchgate.net/publication/343062917_New_Dating_of_the_Piaotang_Granite_and_Related_Tungsten_Mineralization_in_Southern_Jiangxi 陈广文, 李基, 1992. 樟东坑矿床赋存特征及开采损失统计分析. 南方冶金学院学报, 13(4): 271-278. https://www.cnki.com.cn/Article/CJFDTOTAL-NFYX199204000.htm 陈润生, 李建威, 曹康, 等, 2013. 闽北上房钨矿床锆石U-Pb和辉钼矿Re-Os定年及其地质意义. 地球科学——中国地质大学学报, 38(2): 289-304. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201302010.htm 陈郑辉, 王登红, 屈文俊, 等, 2006. 赣南崇义地区淘锡坑钨矿的地质特征与成矿时代. 地质通报, 25(4): 496-501. doi: 10.3969/j.issn.1671-2552.2006.04.013 杜安道, 屈文俊, 王登红, 等, 2007. 辉钼矿亚晶粒范围内Re和187Os的失耦现象. 矿床地质, 26(5): 572-580. doi: 10.3969/j.issn.0258-7106.2007.05.010 杜安道, 赵敦敏, 王淑贤, 等, 2001. Carius管溶样和负离子热表面电离质谱准确测定辉钼矿铼-锇同位素地质年龄. 岩矿测试, 20(4): 247-252. doi: 10.3969/j.issn.0254-5357.2001.04.002 丰成友, 丰耀东, 许建祥, 等, 2007a. 赣南张天堂地区岩体型钨矿晚侏罗世成岩成矿的同位素年代学证据. 中国地质, 34(4): 642-650. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZI200704014.htm 丰成友, 许建祥, 曾载淋, 等, 2007b. 赣南天门山-红桃岭钨锡矿田成岩成矿时代精细测定及其地质意义. 地质学报, 81(7): 952-963. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200707010.htm 付建明, 李华芹, 屈文俊, 等, 2008. 粤北始兴地区石英脉型钨矿成矿时代的确定及其地质意义. 大地构造与成矿学, 32(1): 57-62. doi: 10.3969/j.issn.1001-1552.2008.01.008 古菊云, 1981. 华南钨矿床的形态分带. 见: 余鸿彰著, 钨矿地质讨论会论文集. 北京: 地质出版社, 35-45. 贺礼泰, 2003. 浅议矿脉变化规律与探矿方法. 中国钨业, 18(4): 15-19. doi: 10.3969/j.issn.1009-0622.2003.04.006 胡东泉, 华仁民, 李光来, 等, 2011. 赣南茅坪钨矿流体包裹体研究. 高校地质学报, 17(2): 327-336. doi: 10.3969/j.issn.1006-7493.2011.02.018 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 华仁民, 张文兰, 李光来, 等, 2008. 南岭地区钨矿床共(伴)生金属特征及其地质意义初探. 高校地质学报, 14(4): 527-538. doi: 10.3969/j.issn.1006-7493.2008.04.006 黄小娥, 李光来, 郭家松, 等, 2012. 赣南樟东坑钨矿成矿花岗岩及矿化特征. 地质与勘探, 48(4): 685-692. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKT201204004.htm 李超, 曲文俊, 杜安道, 2009. 大颗粒辉钼矿Re-Os同位素失耦现象及187Os迁移模式研究. 矿床地质, 28 (5): 707-712. doi: 10.3969/j.issn.0258-7106.2009.05.016 李光来, 华仁民, 黄小娥, 等, 2011a. 赣中下桐岭钨矿辉钼矿Re-Os年龄及其地质意义. 矿床地质, 30(6): 1075-1084. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ201106009.htm 李光来, 华仁民, 韦星林, 等, 2011b. 江西中部徐山钨铜矿床单颗粒白云母Rb-Sr等时线定年及其地质意义. 地球科学——中国地质大学学报, 36(2): 282-288. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201102014.htm 刘珺, 叶会寿, 谢桂青, 等, 2008. 江西武功山地区浒坑钨矿床辉钼矿的Re-Os年龄及其地质意义. 地质学报, 82(11): 1576-1584. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200811014.htm 刘英俊, 马东升, 1987. 钨的地球化学. 北京: 科学出版社. 马东升, 2009. 钨的地球化学研究进展. 高校地质学报, 15(1): 19-34. doi: 10.3969/j.issn.1006-7493.2009.01.002 屈文俊, 杜安道, 2003. 高温密闭溶样电感耦合等离子体质谱准确测定辉钼矿铼-锇地质年龄. 岩矿测试, 22(4): 254-262. doi: 10.3969/j.issn.0254-5357.2003.04.003 盛继福, 2004. 钨矿床. 见: 赵一鸣, 吴良士, 白鸽, 等著. 中国主要金属矿床成矿规律. 北京: 地质出版社, 125. 谭运金, 2000. 论南岭地区黑钨矿山的二轮找矿. 中国钨业, 15(6): 9-13. doi: 10.3969/j.issn.1009-0622.2000.06.005 王登红, 陈郑辉, 陈毓川, 等, 2010. 我国重要矿产地成岩成矿年代学研究新数据. 地质学报, 84(7): 1030-1040. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201007009.htm 王小飞, 戚华文, 胡瑞忠, 等, 2010. 粤北红岭钨矿中辉钼矿Re-Os同位素年代学及其地质意义. 矿床地质, 29(3): 415-426. doi: 10.3969/j.issn.0258-7106.2010.03.004 韦星林, 2001. 依靠科技进步开创钨矿地质找矿新局面. 中国钨业, 16(5): 65-68. doi: 10.3969/j.issn.1009-0622.2001.05.019 韦星林, 2012. 赣南钨矿成矿特征与找矿前景. 中国钨业, 27(1): 14-21. doi: 10.3969/j.issn.1009-0622.2012.01.004 吴永乐, 梅勇文, 刘鹏程, 等, 1987. 西华山钨矿地质. 北京: 地质出版社. 夏宏远, 梁书艺, 1986. 南岭某些钨锡(铌钽)矿床的原生分带及成因系列研究. 矿物岩石: 1: 1-182. https://www.cnki.com.cn/Article/CJFDTOTAL-KWYS198601000.htm 幸世军, 陈冬生, 李光来, 2010. 江西樟东坑钨钼矿床"上钨下钼"垂向分带规律浅析. 中国钨业, 25(5): 8-12. doi: 10.3969/j.issn.1009-0622.2010.05.002 杨增海, 王建平, 刘家军, 等, 2012. 内蒙古乌日尼图钨钼矿床成矿流体特征及地质意义. 地球科学——中国地质大学学报, 37(6): 1268-1278. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201206024.htm 曾载淋, 张永忠, 朱祥培, 等, 2009. 赣南崇义地区茅坪钨锡矿床铼-锇同位素定年及其地质意义. 岩矿测试, 28(3): 209-214. doi: 10.3969/j.issn.0254-5357.2009.03.003 张家菁, 陈郑辉, 王登红, 等, 2008. 福建行洛坑大型钨矿的地质特征、成矿时代及其找矿意义. 大地构造与成矿学, 32(1): 92-97. doi: 10.3969/j.issn.1001-1552.2008.01.012 张文兰, 华仁民, 王汝成, 等, 2009. 赣南漂塘钨矿花岗岩成岩年龄与成矿年龄的精确测定. 地质学报, 83(5): 659-670. doi: 10.3321/j.issn:0001-5717.2009.05.007 -
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