Rb-Sr Isochron Age and Its Geological Significance of Baishaziling Tin Deposit in Dayishan Ore Field, Hunan Province
-
摘要: 大义山矿田处于华南褶皱带南岭成矿带中段北缘，位于阳明山－大义山－上堡东西向基底断裂、攸县－宁远北东向基底断裂和郴州－邵阳北西向隐伏深断裂带的交汇部位，主要受大义山岩体控制，其中云英岩脉型锡矿为该矿田典型的成矿类型之一.对该矿田白沙子岭锡矿床云英岩脉型锡矿脉中的石英进行了流体包裹体Rb-Sr同位素测年及其地质意义的讨论.结果显示，矿脉中石英流体包裹体Rb-Sr同位素等时线年龄为160±1 Ma，属于南岭地区中生代160~150 Ma时段成矿高峰期产物；成矿与大义山岩体中侏罗世二长花岗岩具有密切的时间、空间和成因联系，为该期岩浆晚期热液成矿作用的产物；流体包裹体Rb-Sr同位素87Sr/86Sr初始比值为0.706 79±0.003 66，预示其成矿流体有幔源物质的参与，具有地壳和地幔混合流体的特征.Abstract: Dayishan ore field located in the north rim of the middle section of the Nanling metallogenic belt in South China fold zone, and at the intersection of Yangmingshan-Dayishan-Shangpu EW basement fault, Youxian-Ningyuan NE basement fault and Chenzhou-Shaoyang NW concealed deep fault, has been controlled by the Dayishan intrusive rock. The greisens-vein type tin deposit is one of the typical mineralization types in this ore field. The Rb-Sr geochronology of fluid inclusions in quartz of the ore veins is presented and its geological significance of the Baishaziling greisens-vein type tin deposit is discussed in this paper. The Rb-Sr isotopic dating of fluid inclusions of quartz is 160±1 Ma, which indicates that the tin deposit was likely formed in the peaks (160-150 Ma) of Mesozoic mineralization period of Nanling region, and the mineralization was closely related to the magmatic intrusion of the Middle Jurassic monzogranite of Dayishan intrusive rock, as a result of the post-magmatic hydrothermal mineralization. The initial 87Sr/86Sr value of the fluid inclusions is 0.706 79±0.003 66, which may indicate a mantle-derived fluid contribution to the ore-forming fluids.
-
Key words:
- Rb-Sr /
- isotopes /
- quartz fluid inclusion /
- monzogranite /
- geochronology /
- mineral deposit
-
图 1 大义山矿田区域位置(据陈庆等，2005)
1.侏罗系－白垩系；2.泥盆系－三叠系；3.震旦系－奥陶系；4.花岗岩体；5.深大断裂带及编号；6.级构造单元分界线；7.主要断裂及编号；8.典型内生金属矿产.主要断裂名称：(1)NE向宁远－常宁深大断裂带；(2)EW向九嶷山－大东山基底褶皱带；(3)NW向郴州－邵阳断裂带；①阳明山－大义山－上堡东西向基底断裂；②攸县－宁远北东向基底断裂；③郴州－邵阳北西向隐伏深断裂带
Fig. 1. Geological sketch map of the Dayishan ore field
图 2 湘南大义山矿田锡多金属矿产地质简图(伍光英等，2005)
D-P.泥盆系－二叠系; .震旦系－寒武系; J3ηγ.晚侏罗世二长花岗岩; J2ηγ.中侏罗世二云二长花岗岩; J2βηγ.中侏罗世黑云二长花岗岩; J1βkγ.早侏罗世黑云钾长花岗岩; 1.地质界线; 2.左行走滑断裂; 3.大型矿床; 4.中小型矿床; 5.白沙子岭矿区
Fig. 2. The geological sketch map of the tin-polymetallic deposits in the Dyishan ore field, southern Hunan Province
图 3 大义山地区白沙子岭锡矿床地质简图(据曾志方等, 2008)
1.第四系地层；2.马兰边组；3.孟公坳组；4.中侏罗世二云二长花岗岩; 5.中侏罗世黑云二长花岗岩; 6.矽卡岩; 7.取样位置及编号; 8.锡矿脉及编号; 9.断层
Fig. 3. The geological map of the Baishaziling tin deposit in the Dayishan ore field
图 4 白沙子岭锡矿床典型矿石及镜下典型矿物照片
a.石英－锡石－电气石脉型矿石; b.石英－锡石－毒砂脉型矿石; c.含矿云英岩脉; d.毒砂(Apy)、锡石(Cst)共生; e.黄铜矿(Ccp)、锡石(Cst)共生; f.黝锡矿(Sta)、闪锌矿(Sp)与黄铜矿(Ccp)共生
Fig. 4. Photos of typical ores and microscopic images of typical minerals in the Baishaziling tin deposit
图 5 白沙子岭锡矿床云英岩脉型锡矿体中石英流体包裹体Rb-Sr等时线
Fig. 5. Rb-Sr isochron of fluid inclusion in quartzes from the greisen vein orebody of the Baishaziling tin deposit
表 1 大义山岩体岩性及年龄数据
Table 1. The Lithology and chronology of Dayishan intrusive rock
时代 代号 岩性 年龄(Ma) 测试方法 数据来源 晚侏罗世 J3ηγ 中细－细(微)粒二长花岗岩 141，143，144 B 湖南地质矿产勘查局，湖南1∶5万白沙镇幅区域地质调查报告，1988；伍光英等，2005 中侏罗世 J2ηγ 细粒(少斑)二云二长花岗岩 156 B 伍光英等, 2005 J2βηγ 中粗－细(微)粒斑状黑云二长花岗岩 169，181，177 B 湖南地质矿产勘查局，湖南1∶5万白沙镇幅区域地质调查报告，1988；伍光英等, 2005 早侏罗世 J1βkγ 中－细粒斑状(含角闪石)黑云钾长花岗岩 174 Z 湖南地调院，湖南1∶5万罗家桥幅、阳嘉洲幅区域地质调查报告，2000 注：B.黑云母K-Ar法；Z.独居石U-Pb模式年龄. 
下载: 导出CSV
表 2 大义山矿田白沙子岭锡矿床云英岩脉型矿体中石英流体包裹体Rb-Sr同位素组成
Table 2. Rb-Sr isotopic compositions of fluid inclusion in quartzes from the greise vein type orebody of the Baishaziling tin deposit
序号 样品编号 矿物 Rb(10-6) Sr(10-6) 87Rb/86Sr 87Sr/86Sr(2σ) t(Ma) 1 Rb-1 石英 0.412 6 0.041 7 28.75 0.775 89±0.000 04 160±1(1σ) 2 Rb-2 石英 3.647 0 0.058 2 188.10 1.126 82±0.000 04 3 Rb-3 石英 4.205 0 0.047 3 272.00 1.330 66±0.000 07 4 Rb-4 石英 1.010 0 0.043 7 67.59 0.856 17±0.000 05 5 Rb-5 石英 5.618 0 0.159 4 104.00 0.949 13±0.000 06 6 Rb-6 石英 3.988 0 0.075 3 157.90 1.058 22±0.000 10 7 Rb-7 石英 6.198 0 0.058 9 325.30 1.451 28±0.000 08 8 Rb-8 石英 1.940 0 1.760 0 3.18 0.718 72±0.000 05 9 Rb-9 石英 5.594 0 0.103 0 162.20 1.071 34±0.000 06
下载: 导出CSV
表 3 湘南地区部分花岗岩体及钨锡多金属矿床成岩成矿年龄
Table 3. Rock-forming and ore-forming ages of some tungsten-tin polymetallic deposits in southern Hunan Province
矿区 岩体 成岩年龄(Ma) 成矿年龄(Ma) 测试方法 文献 大义山 大义山岩体 160±1 石英Rb-Sr等时线年龄 本文 黄沙坪 花岗斑岩 162 LA-ICPMS锆石U-Pb年龄 姚军明等, 2005 黄沙坪 花岗斑岩 153.8±4.8 辉钼矿Re-Os等时线年龄 马丽艳等，2007 黄沙坪 花岗斑岩 154.8±1.9 辉钼矿Re-Os等时线年龄 姚军明等，2005 金船塘 千里山岩体 133.4±5.9 石英Rb-Sr等时线年龄 马丽艳等，2010 金船塘 千里山岩体 141±11 符山石、石榴石Sm-Nd等时线年龄 马丽艳等，2010 金船塘 千里山岩体 164±12 辉铋矿－黄铁矿Pb-Pb等时线年龄 肖红全等，2003 金船塘 千里山岩体 158.8±6.6 辉钼矿Re-Os等时线年龄 刘晓菲等，2012 红旗岭 千里山岩体 143.1±8.7 石英Rb-Sr等时线年龄 马丽艳等，2010 红旗岭 千里山岩体 155~151 153.3±1 白云母Ar-Ar坪年龄 袁顺达等，2012 柿竹园 千里山岩体 151.1±3.5 辉钼矿Re-Os等时线年龄 李红艳等, 1996 瑶岗仙 瑶岗仙岩体 154.9±2.6 辉钼矿Re-Os等时线年龄 Peng et al., 2006 瑶岗仙 瑶岗仙岩体 153.0±1.1 金云母Ar-Ar坪年龄 Peng et al., 2006 瑶岗仙 瑶岗仙岩体 155.1±1.1 白云母Ar-Ar坪年龄 Peng et al., 2006 香花岭 香花岭岩体 151.9±3 白云母Ar-Ar等时线年龄 Yuan et al., 2007 香花岭 香花岭岩体 160.0±3.2 白云母Ar-Ar等时线年龄 Yuan et al., 2007 香花岭 香花岭岩体 160.3±3.2 白云母Ar-Ar等时线年龄 Yuan et al., 2007 大坳 九嶷山岩体 151.3±2.4 辉钼矿Re-Os等时线年龄 付建明等, 2007 骑田岭 骑田岭岩体 155.5±1.3 锆石SHRIMP U-Pb年龄 赵葵东等，2006 骑田岭 骑田岭岩体 157.1±1.2 锆石SHRIMP U-Pb年龄 赵葵东等，2006 骑田岭 角闪黑云花岗岩 157.5±0.3 黑云母Ar-Ar坪年龄 毛景文等, 2004b 骑田岭 三门锡矿 156.1±0.4 白云母Ar-Ar坪年龄 毛景文等, 2004b 骑田岭 淘洗窝锡矿 160.1±0.9 白云母Ar-Ar坪年龄 毛景文等, 2004b 白腊水
骑田岭岩体南溪单元 146±10 Rb-Sr等时线年龄 李华芹等，2006 含矿花岗斑岩体 146±5 锆石SHRIMP U-Pb年龄 李华芹等，2006 主花岗岩体 155±6 锆石SHRIMP U-Pb年龄 李华芹等，2006 矿化花岗岩 156±5 锆石SHRIMP U-Pb年龄 李华芹等，2006 矿化花岗岩 137±5 Rb-Sr等时线年龄 李华芹等，2006 矿化花岗岩 133±15 Sm-Nd等时线年龄 李华芹等，2006
下载: 导出CSV
-
Cai, M.H., Liang, T., Wei, K.L., et al., 2006. Rb-Sr Dating of the No. 92 Orebody of the Tongkeng-Changpo Deposit in the Dachang Tin-Polymetallic Ore Field, Guangxi, and Its Significance. Geology and Mineral Resources of South China, (2): 31-36(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HNKC200602005.htm Changkakoti, A., Gray, J., Krstic, D., et al., 1988. Determination of Radiogenic Isotope (Rb/Sr, Sm/Nd and Pb/Pb) in Fluid Inclusion Water: An Example from the Bluebell Pb-Zn Deposit, British Columbia, Canada. Geochimica et Cosmochimica Acta, 52: 1961-1967. doi: 10.1016/0016-7037(88)90251-7 Chen, Q., Xu, H.C., He, Z.H., et al., 2005. Ore-Controlling Features of Qianlishan-Dayishan-Jiuyishan Triangle Mineralization Region, Hunan Province. Geology and Mineral Resources of South China, (1): 31-36, 46(in Chinese with English abstract). http://search.cnki.net/down/default.aspx?filename=HNKC200501005&dbcode=CJFD&year=2005&dflag=pdfdown Faure, G., 1986. Principles of Isotope Geology. John Wiley Sons (2nd Edition), New York, 183-199. Fu, J.M., Li, H.Q., Qu, W.J., et al., 2007. Re-Os Isotope Dating of the Da'ao Tungsten-Tin Deposit in the Jiuyi Mountains, Southern Hunan Province. Geology in China, 34(4): 651-656 (in Chinese with English abstract). http://www.researchgate.net/publication/279587596_Re-Os_isotope_dating_of_the_Da'ao_tungsten-tin_deposit_in_the_Jiuyi_Mountains_southern_Hunan_Province Fu, J.M., Xu, D.M., Yang, X.J., et al., 2011. Tin Deposits in Nanling Range. China University of Geosciences Press, Wuhan (in Chinese). Gong, S.Q., Huang, G.F., Hu, Z.K., et al., 2002. Types and Exploration Prospecting of Tin Deposits in Southeastern Dayishan Granite Body. Geology and Mineral Resources of South China, (1): 67-72 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HNKC200201012.htm Hua, R.M., 2005. Differences between Rock-Forming and Related Ore-Forming Times for the Mesozoic Granitoids of Crust Remelting Types in the Nanling Range, South China, and Its Geological Significance. Geological Review, 51(6): 633-639 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP200506005.htm Jiang, S.Y., Zhao, K.D., Jiang, Y.H., et al., 2006. New Type of Tin Mineralization Related to Granite in South China: Evidence from Mineral Chemistry, Element and Isotope Geochemistry. Acta Petrologica Sinica, 22(10): 2509-2516 (in Chinese with English abstract). http://www.oalib.com/paper/1471412 Li, H.Q., Liu, J.Q., Wei, L., 1993. Geochronology and Geologic Application of Fluid Inclusions in Hydrothermal Ore Deposits. Geol. Pub. House, Beijing, 1-27 (in Chinese). Li, H.Q., Lu, Y.F., Wang, D.H., et al., 2006. Dating of the Rock-Forming and Ore-Forming Ages and Their Geological Significances in the Furong Ore-Field, Qitian Mountain, Hunan. Geological Review, 52(1): 113-121 (in Chinese with English abstract). http://www.researchgate.net/publication/284411783_Dating_of_the_rock-forming_and_ore-forming_ages_and_their_geological_significances_in_the_Furong_ore-field_Qitian_Mountain_Hunan Li, H.Y., Mao, J.W., Sun, Y.L., et al., 1996. Re-Os Isotopic Chronology of Molybdenites in the Shizhuyuan Polymetallic Tungsten Deposit, Southern Hunan. Geological Review, 42(3): 261-267 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP199603010.htm Li, Z.L., Hu, R.Z., Peng, J.T., et al., 2006. Helium Isotope Composition of Fluid Inclusions and the Origin of Ore-Forming Fluids of Furong Tin Orefield in Hunan Province, China. Earth Science—Journal of China University of Geosciences, 31(1): 129-135 (in Chinese with English abstract). Liu, S.B., Wang, D.H., Chen, Y.C., et al., 2008. 40Ar/39Ar Ages of Muscovite from Different Types Tungsten-Bearing Quartz Veins in the Chong-Yu-You Concentrated Mineral Area in Gannan Region and Its Geological Significance. Acta Geologica Sinica, 82(7): 932-940 (in Chinese with English abstract). http://www.researchgate.net/publication/279652096_40Ar39Ar_ages_of_muscovite_from_different_types_tungsten-bearing_quartz_veins_in_the_Chong-Yu-You_concentrated_mineral_area_in_Gannan_region_and_its_geological_significance Liu, T.S., 2002. Geological Characteristics and Genesis of Rock Body-Type Tin Deposits in the Dayishan Ore Field. Geology in China, 29(4): 411-415(in Chinese with English abstract). http://d.wanfangdata.com.cn/Periodical/zgdizhi200204015 Liu, X.F., Yuan, S.D., Wu, S.H., 2012. Re-Os Dating of the Molybdenite from the Jinchuantang Tin-Bismuth Deposit in Hunan Province and Its Geological Significance. Acta Petrologica Sinica, 28(1): 39-51 (in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTotal-YSXB201201006.htm Liu, Y.M., Dai, T.M., Lu, H.Z., et al., 1997. 40Ar-39Ar and Sm-Nd Isotope Dating of Rocking, Ore-Forming of the Qianlishan Granites. Science in China (Series D), 27(5): 425-430 (in Chinese). Liu, Y.R., Kuang, J., Ma, T.Q., et al., 2005. 40Ar-39Ar Dating of Biotite in South Dayishan Granite and Its Geological Significance. Resources Survey & Environment, 26(4): 244-249 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HSDZ200504001.htm Lu, Y.F., 2004. GeoKit—A Geochemical Toolkit for Microsoft Excel. Geochimica, 33(5): 459-464 (in Chinese with English abstract). http://ci.nii.ac.jp/naid/10030173896 Ludwig, K., 1999. Isoplot/Ex. Version 2.0: A Geochronological Toolkit for Microsoft Excel. Geochronology Center Special Publication, Berkeley, 1a: 47. Ma, L.Y., Lu, Y.F., Fu, J.M., et al., 2010. The Rb-Sr and Sm-Nd Geochronology Constraints on the Formation Age of Jinchuantang and Hongqiling Tin-Polymetallic Deposits in Dongpo Orefield, Hunan Province. Geology and Mineral Resources of South China, (4): 23-29 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HNKC201004004.htm Ma, L.Y., Lu, Y.F., Qu, W.J., et al., 2007. Re-Os Isotopic Chronology of Molybdenites in Huangshaping Lead-Zinc Deposit, Southeast Hunan, and Its Geological Implications. Mineral Deposits, 26(4): 425-431 (in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTotal-KCDZ200704007.htm Mao, J.W., 1997. Metallogenic Speciality of Super Giant Polymetallic Tungsten Deposit: Taking the Shizhuyuan Deposit as an Example. Scientia Geologica Sinica, 32(3): 351-363 (in Chinese with English abstract). http://dzkx.org/CN/article/downloadArticleFile.do?attachType=PDF&id=9936 Mao, J.W., Xie, G.Q., Li, X.F., et al., 2004a. Mesozoic Large Scale Mineralization and Multiple Lithospheric Extension in South China. Earth Science Frontiers, 11(1): 45-55 (in Chinese with English abstract). Mao, J.W., Li, X.F., Lehmann, B., et al., 2004b. 40Ar-39Ar Dating of Tin Ores and Related Granite in Furong Tin Orefield, Hunan Province, and Its Geodynamic Significance. Mineral Deposits, 23(2): 164-175 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KCDZ200402004.htm Norman, D.Z., Lands, G.P., 1983. Source of Mineralizing Components in Hydrothermal Ore Fluids as Evidenced by 87Sr/86Sr and Stable Isotope Data from the Pasto Bueno Deposit, Peru. Econ. Geol., 78: 451-456. doi: 10.2113/gsecongeo.78.3.451 Peng, H.Q., Wu, G.Y., 2000. Determination of "Dayishan-Style Structure" in Southern Hunan and Its Geological Significance. Hunan Geology, 19(2): 87- 89 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HNDZ200002004.htm Peng, J.T., Zhou, M.F., Hu, R.Z., et al., 2006. Precise Molybdenite Re-Os and Mica Ar-Ar Dating of the Mesozoic Yaogangxian Tungsten Deposit, Central Nanling District, South China. Mineralium Deposita, 41(7): 661-669. doi: 10.1007/s00126-006-0084-4 Rossman, G.R., Weis, D., Wasserburg, G.J., 1987. Rb, Sr, Nd and Sm Concentrations in Quartz. Geochimica et Cosmochimica Acta, 51: 2325-2329. doi: 10.1016/0016-7037(87)90286-9 Shepherd, T.J., Darbyshire, D.P.F., 1981. Fluid Inclusion Rb-Sr Isochrons for Dating Mineral Deposits. Nature, 290: 578-579. doi: 10.1038/290578a0 Sun, J.B., Zhang, L.M., Chen, W., et al., 2013. Quartz Rb-Sr Isotopic Dating of Hongshi Gold Deposit in East Tianshan Mountains. Geological Review, 59(2): 383-388 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP201302021.htm Wu, G.Y., Pan, Z.F., Li, J.D., et al., 2005. Geological and Geochemical Characteristics of the Dayishan Granitoids in Southern Hunan and Their Relations to Mineralization. Geology in China, 32(3): 434-442 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DIZI200503012.htm Wu, G.Y., Peng, H.Q., Jia, B.H., 2000. Geological Features and Emplacement Mechanism of the Dayishan Granitic Intrusion in South Hunan. Geology and Mineral Resources of South China, (3): 1-7(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HNKC200003000.htm Xiao, H.Q., Zhao, K.D., Jiang, S.Y., et al., 2003. Lead Isotope Geochemistry and Ore-Forming Age of Jinchuantang Sn-Bi Deposit in Dongpo Ore Field, Hunan Province. Mineral Deposits, 22(3): 264-270 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KCDZ200303007.htm Yao, J.M., Hua, R.M., Lin, J.F., 2005. Zircon LA-ICPMS U-Pb Dating and Geochemical Characteristics of Huangshaping Granite in Southeast Hunan Province, China. Acta Petrologica Sinica, 21(3): 688-696 (in Chinese with English abstract). http://www.researchgate.net/publication/280687801_Zircon_LA-ICPMS_U-Pb_dating_and_geochemical_characteristics_of_Huangshaping_granite_in_southeast_Hunan_province_China Yuan, S.D., Liu, X.F., Wang, X.D., et al., 2012. Geological Characteristics and 40Ar-39Ar Geochronology of the Hongqiling Tin Deposit in Southern Hunan Province. Acta Petrologica Sinica, 28(12): 3787-3797 (in Chinese with English abstract). http://qikan.cqvip.com/Qikan/Article/Detail?id=44405278 Yuan, S.D., Peng, J.T., Shen, N.P., et al., 2007. 40Ar-39Ar Isotopic Dating of the Xianghualing Sn-Polymetallic Orefield in Southern Hunan, China and Its Geological Implications. Acta Geologica Sinica, 81(2): 278-286. doi: 10.1111/j.1755-6724.2007.tb00951.x Zeng, Z.F., Zeng, Z.X., Zeng, Y.H., et al., 2008. Geological and Geochemical Characteristics and Genesis of the Baishaziling Tin Deposit, Guiyang County, Hunan. Geology in China, 35(4): 725-737 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DIZI200804018.htm Zhao, K.D., Jiang, S.Y., Jiang, Y.H., et al., 2006. SHRIMP U-Pb Dating of the Furong Unit of Qitangling Granite from Southeast Hunan Province and Their Geological Implications. Acta Petrologica Sinica, 22(10): 2611-2616 (in Chinese with English abstract). Zhao, K.D., Jiang, S.Y., Yang, S.Y., et al., 2012. Mineral Chemistry, Trace Elements and Sr-Nd-Hf Isotope Geochemistry and Petrogenesis of Cailing and Furong Granites and Mafic Enclaves from the Qitianling Batholith in the Shi-Hang Zone, South China. Gondwana Research, 22: 310-324. doi:101.1016/j.gr.2011.09.010 Zhou, H.X., Yang, G.H., Jiang, Z.H., et al., 2005. Geological Characteristics and Origin of the Dayishan Tin Orefield in Nanling Region. Geology and Mineral Resources of South China, (2): 87-94 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HNKC200502011.htm Zou, X.W., Cui, S., Qu, W.J., et al., 2009. Re-Os Isotope Dating of the Liguifu Tungsten-Tin Polymetallic Deposit in Dupangling Area, Guangxi. Geology in China, 36(4): 837-844 (in Chinese with English abstract). http://www.researchgate.net/publication/279716361_Re-Os_isotope_dating_of_the_Liguifu_tungsten-tin_polymetallic_deposit_in_Dupangling_area_Guangxi 蔡明海, 梁婷, 韦可利, 等, 2006. 大厂锡多金属矿田铜坑-长坡92号矿体Rb-Sr测年及其地质意义. 华南地质与矿产, (2): 31-36. doi: 10.3969/j.issn.1007-3701.2006.02.006 陈庆, 徐惠长, 何周虎, 等, 2005. 湖南千里山-大义山-九嶷山成矿金三角的控矿意义. 华南地质与矿产, (1): 31-36, 46. https://www.cnki.com.cn/Article/CJFDTOTAL-HNKC200501005.htm 付建明, 李华芹, 屈文俊, 等, 2007. 湘南九嶷山大坳钨锡矿的Re-Os同位素定年研究. 中国地质, 34(4): 651-656. doi: 10.3969/j.issn.1000-3657.2007.04.014 付建明, 徐德明, 杨晓君, 等, 2011. 南岭锡矿. 武汉: 中国地质大学出版社. 龚述清, 黄革非, 胡志科, 等, 2002. 大义山岩体东南部锡矿类型及找矿远景浅析. 华南地质与矿产, (1): 67-72. doi: 10.3969/j.issn.1007-3701.2002.01.012 华仁民, 2005. 南岭中生代陆壳重熔型花岗岩类成岩－成矿的时间差及其地质意义. 地质论评, 51(6): 633-639. doi: 10.3321/j.issn:0371-5736.2005.06.004 蒋少涌, 赵葵东, 姜耀辉, 等, 2006. 华南与花岗岩有关的一种新类型的锡成矿作用: 矿物化学、元素和同位素地球化学证据. 岩石学报, 22(10): 2509-2516. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200610010.htm 李华芹, 刘家齐, 魏琳, 1993. 热液矿床流体包裹体年代学研究及其地质应用. 北京: 地质出版社, 1-27. 李华芹, 路远发, 王登红, 等, 2006. 湖南骑田岭芙蓉矿田成岩成矿时代的厘定及其地质意义. 地质论评, 52(1): 113-121. doi: 10.3321/j.issn:0371-5736.2006.01.015 李红艳, 毛景文, 孙亚莉, 等, 1996. 柿竹园钨多金属矿床的Re-Os同位素等时线年龄研究. 地质论评, 42(3): 261-267. doi: 10.3321/j.issn:0371-5736.1996.03.011 李兆丽, 胡瑞忠, 彭建堂, 等, 2006. 湖南芙蓉锡矿田流体包裹体的同位素组成及成矿流体来源示踪. 地球科学——中国地质大学学报, 31(1): 129-135. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200601017.htm 刘善宝, 王登红, 陈毓川, 等, 2008. 赣南崇义－大余－上犹矿集区不同类型含矿石英中白云母40Ar/39Ar年龄及其地质意义. 地质学报, 82(7): 932-940. doi: 10.3321/j.issn:0001-5717.2008.07.011 刘铁生, 2002. 大义山矿田岩体型锡矿地质特征及矿床成因. 中国地质, 29(4): 411-415. doi: 10.3969/j.issn.1000-3657.2002.04.015 刘晓菲, 袁顺达, 吴胜华, 2012. 湖南金船塘锡铋矿床辉钼矿Re-Os同位素测年及其地质意义. 岩石学报, 28(1): 39-51. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201201006.htm 刘义茂, 戴橦谟, 卢焕章, 等, 1997. 千里山花岗岩成岩成矿的40Ar/39Ar和Sm-Nd同位素年龄. 中国科学(D辑), 27(5): 425-430. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK199705007.htm 刘耀荣, 邝军, 马铁球, 等, 2005. 湖南大义山花岗岩南体黑云母40Ar-39Ar定年及地质意义. 资源调查与环境, 26(4): 244-249. doi: 10.3969/j.issn.1671-4814.2005.04.002 路远发, 2004. GeoKit: 一个用VBA构建的地球化学工具软件包. 地球化学, 33(5): 459-464. doi: 10.3321/j.issn:0379-1726.2004.05.004 马丽艳, 路远发, 屈文俊, 等, 2007. 湖南黄沙坪铅锌多金属矿床的Re-Os同位素等时线年龄及其地质意义, 矿床地质, 26(4): 425-431. doi: 10.3969/j.issn.0258-7106.2007.04.006 马丽艳, 路远发, 付建明, 等, 2010. 湖南东坡矿田金船塘、红旗岭锡多金属矿床Rb-Sr、Sm-Nd同位素年代学研究, 华南地质与矿产, (4): 23-29. doi: 10.3969/j.issn.1007-3701.2010.04.004 毛景文, 1997. 超大型钨多金属矿床成矿特殊性——以湖南柿竹园矿床为例. 地质科学, 32(3): 351-363. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKX703.012.htm 毛景文, 谢桂青, 李晓峰, 等, 2004a. 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): 45-55. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200401002.htm 毛景文, 李晓峰, Bernd Lehmann, 等, 2004b. 湖南芙蓉锡矿床锡矿石和有关花岗岩的40Ar-39Ar年龄及其地球动力学意义. 矿床地质, 23(2): 164-175. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ200402004.htm 彭和求, 伍光英, 2000. 湘南"大义山式构造"的厘定及地质意义. 湖南地质, 19(2): 87-89. https://www.cnki.com.cn/Article/CJFDTOTAL-HNDZ200002004.htm 孙敬博, 张立明, 陈文, 等, 2013. 东天山红石金矿床石英Rb-Sr同位素定年. 地质论评, 59(2): 383-388. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201302021.htm 伍光英, 彭和求, 贾宝华, 2000. 湘南大义山岩体地质特征及其侵位机制分析. 华南地质与矿产, (3): 1-7. https://www.cnki.com.cn/Article/CJFDTOTAL-HNKC200003000.htm 伍光英, 潘仲芳, 李金冬, 等, 2005. 湘南大义山花岗岩地质地球化学特征及其与成矿的关系. 中国地质, 32(3): 434-442. doi: 10.3969/j.issn.1000-3657.2005.03.012 肖红全, 赵葵东, 蒋少涌, 等, 2003. 湖南东坡矿田金船塘锡铋矿床铅同位素地球化学及成矿年龄. 矿床地质, 22(3): 264-270. doi: 10.3969/j.issn.0258-7106.2003.03.007 姚军明, 华仁民, 林锦富, 2005. 湘东南黄沙坪花岗岩LA-ICPMS锆石U-Pb定年及岩石地球化学特征. 岩石学报, 21(3): 688-696. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200503011.htm 袁顺达, 刘晓菲, 王旭东, 等, 2012. 湘南红旗岭锡多金属矿床地质特征及Ar-Ar同位素年代学研究. 岩石学报, 28(12): 3787-3797. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201212001.htm 曾志方, 曾佐勋, 曾永红, 等, 2008. 湖南桂阳县白沙子岭锡矿床地质地球化学特征及其成因. 中国地质, 35(4): 725-737. doi: 10.3969/j.issn.1000-3657.2008.04.017 赵葵东, 蒋少涌, 姜耀辉, 等, 2006. 湘南骑田岭岩体芙蓉超单元的锆石SHRIMP U-Pb年龄及其地质意义. 岩石学报, 22(10): 2611-2616. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200610022.htm 周厚祥, 杨贵花, 蒋中和, 等, 2005. 大义山锡矿田矿床地质特征及矿床成因. 华南地质与矿产, (2): 87-94. doi: 10.3969/j.issn.1007-3701.2005.02.013 邹先武, 崔森, 屈文俊, 等, 2009. 广西都庞岭李贵福钨锡多金属矿Re-Os同位素定年研究. 中国地质, 36(4): 837-844. doi: 10.3969/j.issn.1000-3657.2009.04.010 -
点击查看大图
图(5) / 表(3)
计量
- 文章访问数: 3554
- HTML全文浏览量: 555
- PDF下载量: 426
- 被引次数: 0
