SHRIMP U-Pb Zircon Geochronology of the Jiuling Granitic Complex Batholith in Jiangxi Province
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摘要: 江西九岭花岗岩体产于扬子地块东南缘, 是我国华南的一个规模巨大的复式花岗岩基.该岩体一直被认为是在晋宁期、海西期和燕山期多期次岩浆侵入活动的产物.在对该复式岩基进行详细野外调查的基础上, 开展了锆石SHRIMPUPb年龄测定, 过去认为是晋宁期形成的花岗岩样品, 测出的206Pb/238U年龄为(9828±8) Ma; 而原来认为是海西期形成的甘坊岩体测出的年龄为(820±10) Ma, 说明该区不存在海西期的花岗岩, 结合其他新的年代学资料推测扬子板块内可能不存在加里东—海西期的岩体; 原认为是燕山中期的样品测出的年龄为(151.4±2.4) Ma, 研究结果与原来的一致.此外, 还获得了1.4~1.9 Ga的继承锆石的年龄, 可能代表九岭新元古代花岗岩源岩的年龄.
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关键词:
- 九岭花岗岩 /
- SHRIMP锆石U-Pb年龄 /
- 继承锆石
Abstract: The Jiuling granitic batholith in Jiangxi Province crops out at the southern margin of the Yangtze block, and it is the largest Neoproterozoic granitoid intrusion in South China. The granitic complex has long been considered to consist of Jinningian granites, Hercynian granites and Yanshanian granites. In this paper, a SHRIMP U-Pb zircon geochronological study on this complex has been performed on the basis of detailed field research. The 206Pb/238U age of granite thought to be formed in the Neoproterozoic is (828±8) Ma, while the age of one sample from Ganfang granite thought to be formed in the Hercynian is (820±10) Ma, which suggests there is no Hercynian granite in this area. Combined with other new geochronological data, it seems that there is no proof of Caledonian-Hercynian magmatic activity within the Yangtze block, which may infer that there is no Caledonian-Hercynian intrusion in the interior of the Yangtze block. The age of a sample thought to be formed in the Yanshanian is (151.4±2.4) Ma, which confirms previous results. A few inherited zircons record Mesoproterozoic age information, which may represent the ages of the granite source rocks.-
Key words:
- Jiuling granitic complex /
- SHRIMP U-Pb zircon age /
- inherited zircon
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图 1 九岭花岗岩地质简图及采样点位置
Fig. 1. Sketch geological map of the Jiuling granitic complex and sampling sites
图 2 锆石阴极发光(CL)和背散射(BSE)图像
圈和数字分别表示U-Pb分析点中心和206Pb/238U年龄
Fig. 2. BSE and CL imagings of zircons
图 4 JX03-13和J07锆石SHRIMP U-Pb一致线图解
Fig. 4. Zircon SHRIMP U-Pb concordia diagram of samples JX03-13 and J07
表 1 采样位置及锆石形态特征
Table 1. Sampling positions and morphology of zircons
表 2 九岭花岗岩J39号样的锆石SHRIMP U-Pb分析结果
Table 2. SHRIMP U-Pb data of sample J39 of Jiuling granite
表 3 甘坊花岗岩JX03-13号和九仙塘花岗岩J07的SHRIMPU-Pb锆石年龄分析结果
Table 3. SHRIMP U-Pb data of samples JX03-13 and J07 of Ganfang and Jiuxiantang granites
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Bureau of Geology and Mineral Resources of Jiangxi Province, 1984. Regional geology of Jiangxi Province. Geological Publishing House, Beijing, 399-408 (in Chinese). Group Specially Studying on Granitoids in Nanling Region of the Ministry of Geology and Mineral Resources, 1989. Geology, genesis and mineralization of the granitoids in Nanling region. Geological publishing House, Beijing, 44-248 (in Chinese). Hu, S. L., Wang, S. S., Sang, H. Q., et al., 1985. Anapplication of the fast-neutron activation dating technique to approach the age of early emplacement of Jiuling granodiorite of Jiangxi Province. Acta Petrol. Sinica, 1(3): 29-34 (in Chinese with English abstract). Li, X. H., 1999. U-Pb Zircon ages of granites from the southern margin of the Yangtze craton: Timing of the Neoproterozoic Jinning orogeny in SE China and implications for Rodinia assembly. Precambrian Res. , 97: 43-57. doi: 10.1016/S0301-9268(99)00020-0 Li, X. H., Li, Z. X., Ge, W. C., et al., 2003. Neoproterozoic granitoids in South China: Crustal melting above a mantle plume at Ca. 825 Ma. Precambrian Res. , 122: 45-83. doi: 10.1016/S0301-9268(02)00207-3 Li, X. H., Li, Z. X., Ge, W. C., et al., 2004. Reply to the comment: Mantle plume-but not arc-related Neoproterozoic magmatism in South China. Precambrian Res. , 132: 405-407. doi: 10.1016/j.precamres.2004.03.008 Li, Z. X., Li, X. H., Kinny, P. D., et al., 1999. The breakup of Rodinia: Did it start with a mantle plume beneat South China. Earth Planet. Sci. Lett. , 173: 171-181. doi: 10.1016/S0012-821X(99)00240-X Wan, Y. S., Liu, D. Y., Jian, P., 2004. Comparison between monazite dating and zircon dating. Chinese Science Bulletin, 49(12): 1185-1190 (in Chinese). doi: 10.1360/csb2004-49-12-1185 Wang, X. L., Zhou, J. C., Qiu, J. S., et al., 2004. Geochemistry of the Meso- to Neoproterozoic basic-acid rocks from Hunan Province, South China: Implications for the evolution of the western Jiangnan orogen. Precambrian Res. , 135: 79-103. doi: 10.1016/j.precamres.2004.07.006 Williams, I. S., 1998. U-Th-Pb geochronology by ion microprobe. In: McKibben, M. A., Shanks, W. C., Ridley, W. I., eds., Applications of microanalytical techniques to understanding mineralizing processes. Reviews in Economic Geology, 7: 1-35. Xu, H. J., Ma, C. Q., Zhong, Y. F., et al., 2004. Zircon SHRIMP U-Pb dating of Taojiang and Dashenshan granites in Hunan Province: The lower time limit of collision between Yangtze block and Cathysia block. In: Abstracts of the national proseminar on petrology and geodynamics in 2004.312-314 (in Chinese). Xu, X. S., Zhou, X. M., 1992. Precambrian S-type granitoids in South China and their geological significance. J. Nanjing Univ. (Nat. Sci. Ed. ), 28(3): 424-430 (in Chinese with English abstract). Zhou, J. C., Wang, X. L., Qiu, J. S., et al., 2004. Geochemistry of Meso- and Neoproterozoic mafic-ultramafic rocks from northern Guangxi, China: Arc or magmatism. GeoChem. J. , 38(2): 139-152. doi: 10.2343/geochemj.38.139 Zhou, M. F., Yan, D. P., Kennedy, A. K., et al., 2002. SHRIMP U-Pb zircon geochronological and geochemical evidence for Neoproterozoic arc-magmatism along the western margin of the Yangtze block, South China. Earth Planet. Sci. Lett. , 196: 51-67. doi: 10.1016/S0012-821X(01)00595-7 地矿部南岭项目花岗岩专题组, 1989. 南岭花岗岩地质及其成因和成矿作用. 北京: 地质出版社, 44-248. 胡世玲, 王松山, 桑海清, 等, 1985. 应用40Ar/39Ar快中子活化定年技术探讨江西九岭花岗岩早期侵位时代. 岩石学报, 1(3): 29-34. http://www.cnki.com.cn/Article/CJFDTotal-YSXB198503002.htm 江西省地质矿产局, 1984. 江西省区域地质志. 北京: 地质出版社, 399-408. 万渝生, 刘敦一, 简平, 2004. 独居石和锆石SHRIMP U-Pb定年对比. 科学通报, 49(12): 1185-1190. doi: 10.3321/j.issn:0023-074X.2004.12.013 徐夕生, 周新民, 1992. 华南前寒武S型花岗岩类及其地质意义. 南京大学学报(自然科学版), 28(3): 424-430. https://www.cnki.com.cn/Article/CJFDTOTAL-NJDZ199203010.htm 续海金, 马昌前, 钟玉芳, 等, 2004. 湖南桃江、大神山花岗岩的锆石SHRIMP定年: 扬子与华夏拼合的时间下限. 见: 2004年全国岩石学与地球动力学研讨会论文摘要. 312-314. -
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