Geochemical and Zircon Hf Isotopic Characteristics of Mesozoic Intermediate-Acid Intrusive Rocks in Shujiadian Area, Tongling and Their Geological Significance
-
摘要: 通过锆石LA-MC-ICP-MS Lu-Hf同位素分析，结合前人地球化学资料对舒家店地区中酸性侵入岩进行了研究.主量、微量元素地球化学特征表明区内侵入岩为准铝质，具有岛弧岩浆岩的特征，区内岩浆的演化可能经历了同化混染与分离结晶（AFC）过程.通过分析，我们认为舒家店地区的早白垩世岩浆活动可能与早白垩世初太平洋板块的斜向俯冲相关，侵入岩的形成演化受到了区域构造应力场的制约.Hf同位素分析及计算结果表明，除两个继承性锆石核外，本区侵入岩锆石的εHf（t）均为负值，橄榄安粗岩系列侵入岩的εHf（t）值为-8.6~-4.1，高钾钙碱性系列εHf（t）值为-13.4~-4.7.与高钾钙碱性系列相比，橄榄安粗岩系列侵入岩的εHf（t）更接近球粒陨石演化线.从εHf（t）值的变化特征来看，两个系列侵入岩均为来源于富集地幔，且在演化过程中混染了地壳物质，而高钾钙碱性系列在这个过程中混入了更多的地壳物质.Abstract: In this paper, we carry out research on intermediate-acid intrusive rocks in Shujiadian area in aspect of zircon LA-MC-ICP-MS Lu-Hf isotopes combining previous geochemical data. The characteristics of major and trace elements show that the rocks belong to metaluminous series with attributes of island arc magmatic rocks, and may have experienced assimilation-fractional crystallization (AFC) process. We considered that the Early Cretaceous magmatic activity might relate to the oblique subduction of the Pacific plate in the beginning of the Cretaceous, and the evolution of the intrusive rocks in the area were subject to the regional tectonic stress field. The Hf isotope analysis shows that except two inherited zircon cores, the εHf(t) values are negative, with shoshonite series being -8.6 to -4.1 and High-K calc-alkaline series -13.4 to -4.7. Comparing to the high-K calc-alkaline series rocks, the εHf(t) values of the shoshonite series are closer to chondrite evolution line. Considering from the variance of εHf(t) values for the two series, though they both originated from enriched mantle and were contaminated with crustal material during magmatic evolution, the high-K series was contaminated more during this process.
-
Key words:
- Shujiadian /
- geochemistry /
- zircon Hf isotope /
- tectonic setting /
- material source
-
图 1 铜陵地区构造-岩浆岩分布
N.新近系；K2.上白垩统；K1.下白垩统；J3.上侏罗统；J1-2.下中侏罗统；T22-T23.中三叠统；D3-T21.上泥盆统-下中三叠统；S.志留系；其中（b）据吴才来等（2013）
Fig. 1. Sketch map of distribution of tectonics-igneous rocks in Tongling area
图 2 舒家店侵入岩分布图
据华东冶金地质勘察研究院内部资料修改
Fig. 2. Distribution of intrusive rocks in Shujiadian area
图 3 舒家店地区钻孔岩心柱状图及采样位置
Fig. 3. Sketch of drill holes in Shujiadian area and sampling positions
图 5 舒家店中酸性侵入岩QAP图解
▲橄榄安粗岩系列；△高钾钙碱性系列；数据李进文等（2004）；王世伟等（2011）；吴才来等（2013）；李名则等（2016）
Fig. 5. QAP triangular diagram of intermediate-acid intrusive rocks in Shujiadian area
图 6 舒家店地区中酸性侵入岩哈克图解
数据李进文等（2004）；王世伟等（2011）；吴才来等（2013）；李名则等（2016）
Fig. 6. Harker diagram of intermediate-acid intrusive rocks in Shujiadian area
图 7 舒家店地区中酸性侵入岩哈克图解
标准化数据引自Sun and McDonough（1989）; 数据王世伟等（2011）；吴才来等（2013）；李名则等（2016）
Fig. 7. Spider diagrams of trace elements and REE patterns for shoshonite and calc-alkaline series rocks of Shujiadian area
图 8 舒家店地区中酸性侵入岩构造环境判别图解
底图据Pearce et al.(1984)；▲橄榄安粗岩系列，△高钾钙碱性系列；数据王世伟等（2011）; 吴才来等（2013）; 李名则等（2016）
Fig. 8. Discrimination diagrams of tectonic setting of intermediate-acid intrusive rocks in Shujiadian area
图 9 舒家店地区中酸性侵入岩FAM图解（%）
底图据Pearce et al.(1977)；▲橄榄安粗岩系列，△高钾钙碱性系列；数据李进文等（2004）; 王世伟等（2011）; 吴才来等（2013），李名则等（2016）；Ⅰ.洋中脊或洋底；Ⅱ.洋岛；Ⅲ.大陆；Ⅳ.扩张性中央岛：Ⅴ.造山带
Fig. 9. FeOt-MgO-Al2O3 diagram of intermediate-acid intrusive rocks in Shujiadian area
图 10 舒家店地区中酸性侵入岩La/Yb-δEu图解及Rb/Y-Nb/Y图解
▲橄榄安粗岩系列，△高钾钙碱性系列；数据王世伟等（2011）；吴才来等（2013）；李名则等（2016）; 左图.底图据谢建成(2008); 右图.底图据Chazot and Bertrand（1995）修改
Fig. 10. La/Yb-δEu diagram and Rb/Y-Nb/Y diagram of intermediate-acid intrusive rocks in Shujiadian area
图 11 舒家店地区中酸性侵入岩Hf同位素组成
Fig. 11. Hf isotope composition of intermediate-acid intrusive rocks in Shujiadian area.
图 12 舒家店地区中酸性侵入岩T-εHf(t)及两阶段Hf模式年龄图解
其中宁芜盆地岩浆岩εHf(t)数据侯可军等（2010）；胡劲平等（2010）；陈志洪等（2013）
Fig. 12. Diagrams of T-εHf(t) of intermediate-acid intrusive rocks in Shujiadian area and histogram of two-stage Hf model ages of intrusive rocks of Shujiadian area (lower)
-
[1] Chang, Y.F., Liu, X.P., Wu, Y.C., 1991. The Copper-Iron Belt of the Lower and Midde Reaches of the Changjiang River. Geological Publishing House, Beijing, 1-379 (in Chinese with English abstract). [2] Chazot, G., Bertrand, H., 1995. Genesis of Silicic Magmas during Tertiary Continental Rifting in Yemen. Lithos, 36:69-83. https://doi.org/10.1016/0024-4937(95)00012-5 [3] Chen, Z.H., Guo, K.Y., Zhao, L., 2013. Zircon U-Pb Dating and Hf Isotopic Study on Granitic Intrusions in the Basement of the Ningwu Basin. Bulletin of Mineralogy, Petrology and Geochemistry, 32(6):704-712 (in Chinese). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kwysdqhxtb201306004 [4] Deng, J.F., Zhao, G.C., Zhao, H.L., et al., 2000. Yanshanian Igneous Petrotectonic Assemblage and Orogenic-Deep Processes in East China. Geological Review, 49(1):41-48 (in Chinese with English abstract). https://www.researchgate.net/publication/284972999_Yanshanian_igneous_petrotectonic_assemblage_and_orogenic-deep_process_in_east_China [5] Ding, L.X., Huang, G.C., Xia, J.L., 2018. Age and Petrogenesis of the Echeng Intrusion in Southeastern Hubei Province:Implications for Iron Mineralization. Earth Science, 43(7):2350-2369. http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX201807012.htm [6] Dong, S.W., 1991. Tectonic Analysis on Genesis of Metallogenetic Belt of Middle-Lower Yangtze River. Bulletin of the Chinese Academy of Geological Sciences, 23:43-56 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQXB199102003.htm [7] Gao, G., Xu, Z.W., Yang, X.N., 2006. Petrogenesis of the Baimangshan Pyroxene Diorite Intrusion in Tongling Area, Anhui Province:Constraints from Sr-Nd-Pb-O Isotopes. Journal of Nanjing University (Natrual Sciences), 42(3):269-279 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-NJDZ200603003.htm [8] Gu, L.X., Xu, K.Q., 1986. On the South China Type Massive Sulfide Ore Deposits Formed in Marine Fault Depression troughs on the Continental Crust. Mineral Deposits, 5(2):1-13 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-KCDZ198602000.htm [9] Hou, K.J., Li, Y.H., Zou, T.R., et al., 2007. Laser Ablation-MC-ICP-MS Technique for Hf Isotope Microananlysis of Zircon and Its Geological Applications. Acta Petrologica Sinica, 23(10):2595-2604 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200710026.htm [10] Hou, K.J., Yuan, S.D., 2010. Zircon U-Pb Age and Hf Isotopic Composition of the Volcanic and Sub-Volcanic Rocks in the Ningwu Basin and Their Geological Implications. Acta Petrologica Sinica, 26(3):888-902 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201003020 [11] Hu, J.P., Jiang, S.Y., 2010. Zircon U-Pb Dating and Hf Isotopic Compositions of Porphyrites from the Ningwu Basin and Their Geological Implications. Geological Journal of China Universities, 16(3):294-308 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gxdzxb201003003 [12] Lassiter, J.C., DePaolo, D.J., 2013. Plume/Lithosphere Interaction in the Generation of Continental and Oceanic Flood Basalts:Chemical and Isotopic Constraints. In:Mahoney, J.J., Coffin, M.F., eds., Large Igneous Provinces:Continental, Oceanic, and Planetary Flood Volcanism. American Geophysical Union, Washington, 100:335-355. https://ui.adsabs.harvard.edu/abs/1997GMS...100..335L/abstract [13] Li, J.W., 2004. Ore-Controling Structure of Orefield and Ore-Forming Chemical Kinetics of Mineral assemblage in Tongling(Dissertation). Chinese Academy of Geological Sciences, Beijing, 1-142 (in Chinese with English abstract). [14] Li, M.Z., Wu, C.L., Lei, M., et al., 2016. Zircon U-Pb Geochronology of Intermediate-Acid Intrusions in the Shujiadian Ore District of the Tongling Ore Concentration Area. Geology in China. 43(5):1514-1544(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi201605004 [15] Li, S.G., 2000. Sm-Nd and Rb-Sr Isotopic Chronology and Cooling History of Ultrahigh Pressure Metamorphic Rocks and Their Country Rocks at Shuanghe in the Dabie Mountains, Central China. Geochimica et Cosmochimica Acta. 64(6):1077-1093. doi: 10.1016/S0016-7037(99)00319-1 [16] Mao, J.R., Su, Y.X., Chen, S.Y., 1990. Intermediate Acid Intrusive Rocks and Metallogenesis in the Middle-Lower Reaches of the Yangtze River. Geological Publishing House, Beijing, 1-191 (in Chinese). [17] Pearce, J.A., Harris, N.B.W., Tindle, A.G., 1984. Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks. Journal of Petrology, 25(4):956-983. doi: 10.1093/petrology/25.4.956 [18] Pearce, T.H., Gorman, B.E., Birkett, T.C., 1977. The Relationship between Major Element Chemistry and Tectonic Environment of Basic and Intermediate Volcanic Rocks. Earth and Planetary Science Letters, 36(1):121-132. https://doi.org/10.1016/0012-821X(77)90193-5 https://www.sciencedirect.com/science/article/abs/pii/0012821X77901935 [19] Pei, X.Z., Ding, S.P., Zhang, G.W., et al., 2007. Zircons LA-ICP-MS U-Pb Dating of Neoproterozoic Granitoid Gneisses in the North Margin of West Qinling and Geological Implication. Acta Geologica Sinica, 81(6):772-786 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb200706005 [20] Qu, H.Y., Wang, H.L., Pei, R.F., et al., 2012. Zircon U-Pb Geochronological and Hf Isotopic Constraints on Petrogenesis of Tieshan and Jinshandian Plutons in the Southeastern Hubei Province. Acta Petrologica Sinica, 28 (1):147-165 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201201012 [21] Sun, S.S., McDonough, W.F., 1989. Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes. In:Saunders, A.D., Norry, M.J., eds., Magmatism in the Ocean Basins. Geological Society, London, 42:313-345. https://www.researchgate.net/publication/231575101_Chemical_and_isotopic_systematics_of_oceanic_basalts_Implications_for_mantle_composition_and_processes [22] Sun, W., Ding, X., Hu, Y.H., 2007. The Golden Transformation of the Cretaceous Plate Subduction in the West Pacific. Earth and Planetary Science Letters, 262(3-4):533-542. https://doi.org/10.1016/j.epsl.2007.08.021 [23] Tang, Z.C., Zhou, H.W., Hu, K.M., et al., 2019. Petrogenesis of Late Mesozoic Granites in Northwest Zhejiang. Earth Science, 44(4):1278-1294(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX201904016.htm [24] Wang, Q., Xu, J.F., Zhao, Z.H., et al., 2003. Petrogenesis of the Yanshanian Intrusive Rocks in Tongling Area, Anhui and Its Constraints on Deep Dynamic Process. Science in China (Seiries D), 33(4):323-334 (in Chinese). [25] Wang, S.W., Zhou, T.F., Yuan, F., et al., 2011. Geochronology and Geochemical Characteristics of the Shujiaidian Intrusion in Tongling, China. Acta Geologica Sinica, 85(5):849-861 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb201105018 [26] Wang, S.W., Zhou, T.F., Yuan, F., et al., 2016. Geochemical Characteristics of the Shujiadian Cu Deposit Related Intrusion in Tongling:Petrogenesis and Implications for the Formation of Porphyry Cu Systems in the Middle-Lower Yangtze River Valley Metallogenic Belt, Eastern China. Lithos, 252-253:185-199. https://doi.org/10.1016/j.lithos.2016.02.013 [27] Wang, Y., Deng, J.F., Ji, G.Y., 2004. A Perspective on the Geotectonic Setting of Early Cretaceous Adakite-Like Rocks in the Lower Reaches of Yangtze River and Its Significance for Copper-Gold Mineralization. Acta Petrologica Sinica, 20(2):297-314 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200402011 [28] Wilson, M., 1989. Igneous Petrogenesis: A Global Tectonic Approach. Chapman and Hall, London, 1-466. [29] Wu, C.L., Chen, S.Y., Shi, R.D., et al., 2003. Origin and Features of the Mesozoic Intermediate-Acid Intrusive Rocks in the Tongling Area, Anhui, China. Acta Geoscientia Sinica, 24(1):41-48 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dldlx-e200101001 [30] Wu, C.L., Dong, S.W., Guo. X.Y., 2013. Intermediate-Acid Intrusive Rocks in Tongling, China. Geological Publishing House, Beijing, 1-220 (in Chinese with English abstract). [31] Wu, C.L., Dong, S.W., Wu, D., et al., 2017. Late Mesozoic High-K Calc-Alkaline Magmatism in SE China:The Tongling Example. International Geology Review, 2017(1):1-35. https://doi.org/10.1080/00206814.2017.1313137 [32] Wu, C.L., Gao, Q.M., Guo, H.P., et al., 2010. Petrogenesis of the Intermediate-Acid Intrusive Rocks and Zircon SHRIMP Dating in Tongling, Anhui China. Acta Petrologica Sinica, 26(9):2630-2652(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201009011 [33] Wu, Y.C., Cao, F.Y., Chang, Y.F., 1999. A Preliminary Study on the Deepseated Structural-Magmatic Control over the Metallogenic System around the Yangtze River Reaches in Anhui Province. Earth Science Frontiers, 6(2):92-103 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY902.007.htm [34] Xie, J.C., 2008. The Diagenesis and Metallogenesis Research of Mesozoic Magmatic Rocks in Tongling Region, Anhui Province(Dissertation). University of Science and Technology of China, Heifei, 1-213 (in Chinese with English abstract). [35] Xing, F.M., 1996. Alkaline Source of Mesozoic Magmatic Rocks along the Reaches of the Yangtze River in Anhui Province. Geology of Anhui, 6(1):15-18 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-AHDZ601.002.htm [36] Xu, X.C., Bai, R.Y., Xie, Q.Q., et al., 2012. Reunderstanding of the Geological and Geochemical Characteristics of the Mesozoic Intrusive Rocks from Tongling Area of Anhui Province, and Discussions on Their Genesis. Acta Petrologica Sinica, 28(10):3139-3169 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201210010.htm [37] Yuan, F., Zhou, T.F., Fan, Y., et al., 2011. Zircon U-Pb Ages and Isotopic Characteristics of the Granitoids in the Ningwu Basin, China, and Their Significance. Acta Geologica Sinica, 85(5):821-833 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb201105016 [38] Zhai, Y.S., Yao, S.Z., Lin, X.D., et al., 1992. Metallogenic Regularity of Iron and Copper (Gold) Deposits in the Middle-Lower Reaches of the Yangtze River. Geological Publishing House, Beijing, 1-235 (in Chinese). [39] Zhang, Q., Qang, Y., Qian, Q., et al., 2001. The Characteristics and Tectonic-Metallogenic Significance of the Adakites in Yanshan Period from Eastern China. Acta Petrologica Sinica, 17(2):236-244(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200102007.htm [40] Zhu, G., Liu, G.S., Niu, M.L., et al., 2003. Transcurrent Movement and Genesis of the Tan-Lu Fault Zone. Geological Bulletin of China, 22(3):200-207 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz200303009 [41] 常印佛, 刘湘培, 吴言昌, 1991.长江中下游铜铁成矿带.北京:地质出版社, 1-379. [42] 陈志洪, 郭坤一, 赵玲, 2013.宁芜盆地火山基底侵入岩的锆石U-Pb定年和铪同位素研究.矿物岩石地球化学通报, 32(6):704-712. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kwysdqhxtb201306004 [43] 邓晋福, 赵国春, 赵海玲, 等, 2000.中国东部燕山期火成岩构造组合与造山-深部过程.地质论评, 46 (1):41-48. doi: 10.3321/j.issn:0371-5736.2000.01.006 [44] 丁丽雪, 黄圭成, 夏金龙, 2018.鄂东南地区鄂城岩体的时代、成因及其对成矿作用的指示.地球科学, 43(7):2350-2369. doi: 10.3799/dqkx.2018.569 [45] 董树文, 1991.长江中下游铁铜成矿带之构造分析.中国地质科学院院报, 23:43-56. http://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDJ199100008006.htm [46] 高庚, 徐兆文, 杨小男, 等, 2006.安徽铜陵白芒山辉石闪长岩体的成因:Sr-Nd-Pb-O同位素制约.南京大学学报(自然科学版), 42(3):269-279. doi: 10.3321/j.issn:0469-5097.2006.03.004 [47] 顾连兴, 徐克勤, 1986.论大陆地壳断裂拗陷带中的华南型块状硫化物矿床.矿床地质, 5 (20):1-13. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gxdzxb200304012 [48] 侯可军, 李延河, 邹天人, 等, 2007. LA-MC-ICP-MS锆石Hf同位素的分析方法及地质应用.岩石学报, 23(10):2595-2604. doi: 10.3969/j.issn.1000-0569.2007.10.025 [49] 侯可军, 袁顺达, 2010.宁芜盆地火山-次火山岩的锆石U-Pb年龄、Hf同位素组成及其地质意义.岩石学报, 26(3):888-902. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201003020 [50] 胡劲平, 蒋少涌, 2010.宁芜盆地浅成侵入岩的锆石U-Pb年代学和Hf同位素研究及其地质意义.高校地质学报, 16(3):294-308. doi: 10.3969/j.issn.1006-7493.2010.03.003 [51] 李进文, 2004.铜陵矿集区矿田构造控矿与成矿化学动力学研究(博士学位论文).安徽: 中国科学院大学, 1-152. http://cdmd.cnki.com.cn/Article/CDMD-82501-2007213419.htm [52] 李名则, 吴才来, 雷敏, 等, 2016.铜陵矿集区舒家店矿区中酸性侵入岩锆石U-Pb年代学研究.中国地质, 43(5):1514-1544. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi201605004 [53] 毛建仁, 苏郁香, 陈三元, 1990.长江中下游中酸性侵入岩与成矿.北京:地质出版社, 1-191. [54] 裴先治, 丁仨平, 张国伟, 等, 2007.西秦岭北缘新元古代花岗质片麻岩的LA-ICP-MS锆石U-Pb年龄及其地质意义.地质学报, 81(6):772-786. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb200706005 [55] 瞿泓滢, 王浩琳, 裴荣富, 等, 2012.鄂东南地区与铁山和金山店铁矿有关的花岗质岩体锆石LA-ICP-MS年龄和Hf同位素组成及其地质意义.岩石学报, 28 (1):147-165. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201201012 [56] 唐增才, 周汉文, 胡开明, 等, 2019.浙西北地区晚中生代花岗岩的岩石成因.地球科学, 44(4):1278-1294. doi: 10.3799/dqkx.2018.208 [57] 汪洋, 邓晋福, 姬广义, 2004.长江中下游地区早白垩世埃达克质岩的大地构造背景及其成矿意义.岩石学报, 20(2):297-314. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200402011 [58] 王强, 许继峰, 赵振华, 等, 2003.安徽铜陵地区燕山期侵入岩的成因及其对深部动力学过程的制约.中国科学(D辑:地球科学), 33(4):323-334. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkx-cd200304005 [59] 王世伟, 周涛发, 袁峰, 等, 2011.铜陵舒家店岩体的年代学和地球化学特征研究.地质学报, 85(5):849-861. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb201105018 [60] 吴才来, 陈松永, 史仁灯, 等, 2003.铜陵中生代中酸性侵入岩特征及成因.地球学报, 24(1):41-48. doi: 10.3321/j.issn:1006-3021.2003.01.007 [61] 吴才来, 董树文, 郭祥焱, 等, 2013.中国铜陵中酸性侵入岩.地质出版社, 1-220. [62] 吴才来, 高前明, 国和平, 等, 2010.铜陵中酸性侵入岩成因及锆石SHRIMP定年.岩石学报, 26 (9):2630-2652. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201009011 [63] 吴言昌, 曹奋扬, 常印佛, 1999.初论安徽沿江地区成矿系统的深部构造-岩浆控制.地学前缘, 6(2):92-103. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy199902007 [64] 谢建成, 2008.安徽铜陵地区中生代岩浆岩成岩和成矿作用研究(博士学位论文).安徽: 中国科学技术大学, 1-213. http://cdmd.cnki.com.cn/Article/CDMD-10358-2008091812.htm [65] 邢凤鸣, 1996.安徽沿长江地区中生代岩浆岩的碱质来源.安徽地质, 6(1):15-18. http://www.cnki.com.cn/Article/CJFDTotal-AHDZ601.002.htm [66] 徐晓春, 白茹玉, 谢巧勤, 等, 2012.安徽铜陵中生代侵入岩地质地球化学特征再认识及成因讨论.岩石学报, 28(10):3139-3169. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201210008 [67] 袁峰, 周涛发, 范裕, 等, 2011.宁芜盆地花岗岩类的锆石U-Pb年龄、同位素特征及其意义.地质学报, 85(5):821-833. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb201105016 [68] 翟裕生, 姚书振, 林新多, 等, 1992.长江中下游地区铁铜(金)成矿规律.北京:地质出版社, 1-235. [69] 张旗, 王焰, 钱青, 等, 2001.中国东部燕山期埃达克岩的特征及其构造-成矿意义.岩石学报, 17(2):236-244. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200102008 [70] 朱光, 刘国生, 牛漫兰, 等, 2003.郯庐断裂带的平移运动与成因.地质通报, 22(3):200-207. doi: 10.3969/j.issn.1671-2552.2003.03.009 -
dqkx-45-7-2555-Table1.doc
-
下载:
点击查看大图
图(12)
计量
- 文章访问数: 637
- HTML全文浏览量: 151
- PDF下载量: 38
- 被引次数: 0
