吉林省塔东群锆石U-Pb定年、微量元素研究及其地质意义

孟杰; 刘晓旸; 梁一鸿; 秦亚; 句高; 李本仙

doi:10.3799/dqkx.2017.040

Volume 42 Issue 4

Apr. 2017

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Article Navigation > Earth Science > 2017 > 42(4): 502-510

Meng Jie, Liu Xiaoyang, Liang Yihong, Qin Ya, Ju Gao, Li Benxian, 2017. U-Pb Dating and Trance Elements Composition of Tadong Group from Jilin Province and Their Geological Implications. Earth Science, 42(4): 502-510. doi: 10.3799/dqkx.2017.040

Citation:

Meng Jie, Liu Xiaoyang, Liang Yihong, Qin Ya, Ju Gao, Li Benxian, 2017. U-Pb Dating and Trance Elements Composition of Tadong Group from Jilin Province and Their Geological Implications. Earth Science, 42(4): 502-510. doi: 10.3799/dqkx.2017.040

Citation:

Meng Jie, Liu Xiaoyang, Liang Yihong, Qin Ya, Ju Gao, Li Benxian, 2017. U-Pb Dating and Trance Elements Composition of Tadong Group from Jilin Province and Their Geological Implications. Earth Science, 42(4): 502-510. doi: 10.3799/dqkx.2017.040

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U-Pb Dating and Trance Elements Composition of Tadong Group from Jilin Province and Their Geological Implications

doi: 10.3799/dqkx.2017.040

Meng Jie^{1,2
,},
Liu Xiaoyang¹,
Liang Yihong¹,
Qin Ya³,
Ju Gao¹,
Li Benxian^{1
,
,}

1.
College of Earth Sciences, Jilin University, Changchun130061, China
2.
College of Geographical Science, Harbin Normal University, Harbin150025, China
3.
College of Earth Sciences, Guilin University of Technology, Guilin541004, China

Received Date: 2016-09-12
Publish Date: 2017-04-15

Abstract

Abstract

Tadong Group of Jilin Province is known for large-scale magnetite ore deposit, and Tadong iron deposit is the largest submarine volcano plume-metamorphic-reformation iron deposit in the Jilin-Heilongjiang metallogenic province. Complicated of geological characteristics and geological processes made the ownership of Tadong Group long been controversial. In this paper, the U-Pb zircon ages of the biotite plagioclase gneiss and magnetite diopside plagioclase leptynite are obtained by LA-ICP-MS. Zircons that obtained from biotite plagioclase gneiss are prismatic, and Th/U range between 0.17 and 0.65. U-Pb dating of these zircons record ²⁰⁶Pb/²³⁸U weighted mean age of 517.6±2.7 Ma, indicating the formation age of the vocanic. In the magnetite diopside plagioclase leptynite, there are two kinds of zircons with two age groups, respectively. The first kind of zircons are short columns, and Th/U range between 0.78 and 1.00. U-Pb dating of these zircons record ²⁰⁶Pb/²³⁸U weighted mean age of 249.8±4.0 Ma, indicating the age of thermal disturbance. Another kind of zircons are subhedral short prismatic, and have extremely high U, Th contents, the highest Th contents is 17 422 μg/g, respectively. U-Pb dating of these zircons record ²⁰⁶Pb/²³⁸U weighted mean age of 518.3±3.8 Ma, attributing to the age of hydrothermal event. It is indicated that there is a hydrothermal process at 518.3 Ma or so, which might be related to magmatism. Iron mineralization of Tadong iron deposit of Jilin Province is most likely related with this hydrothermal event. Therefore, one of mineralizations happened in the Early Cambrian Period (±520 Ma) in Tadong iron deposit.
- Tadong Group,
- magmatic zircons,
- hydrothermal zircons,
- U-Pb dating,
- Tadong iron deposit,
- geochemistry

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References(37)

References

Belousova, E.A., Griffin, W.L., O'Reilly, S.Y., et al., 2002.Igneous Zircon:Trace Element Composition as an Indicator of Source Rock Type.Contributions to Mineralogy and Petrology, 143:602-622.doi: 10.1007/s00410-002-0364-7

Corfu, F., Hanchar, J.M., Hoskin, P.W.O., et al., 2003.Altas of Zircon Textures.Reviews in Mineralogy and Geochemistry, 53:469-500.doi: 10.2113/0530469

Geisler, T., Rashwan, A.A., Rahn, M.K.W., et al., 2003.Low-Temperature Hydrothermal Alteration of Natural Metamict Zircons from the Eastern Desert, Egypt.Mineralogical Magazine, 67(3):485-508.doi: 10.1180/0026461036730112

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.doi: 10.1016/j.gca.2004.07.006

Hoskin, P.W.O., Schaltegger, U., 2003.The Composition of Zircon and Igneous and Metamorphic Petrogenesis.Reviews in Mineralogy and Geochemistry, 53(1):27-62.doi: 10.2113/0530027

Hoskin, P.W.O., Ireland, T.R., 2000.Rare Earth Element Chemistry of Zircon and Its Use as a Provenance Indicator.Geology, 28(7):627-630.doi:10.1130/0091-7613(2000)28<627:REECOZ>2.0.CO; 2

Hu, Z.C., Gao, S., Liu, Y.S., et al., 2008.Signal Enhancement in Laser Ablation ICP-MS by Addition of Nitrogen in the Central Channel Gas.Journal of Analytical Atomic Spectrometry, 23(8):1093-1101.doi: 10.1039/b804760j

Koschek G., 1993.Origin and Significance of the SEM Cathodoluminescence from Zircon.Microscopy, 171:223-232.doi: 10.1111/j.1365-2818.1993.tb03379.x

Kou, L.L., Zhang, S., Lü, J.C., et al., 2013.Geochemical Characteristics and Tectonic Implication of the Iron Ore Formation in Tadong Area, Jilin Province.Geology and Resources, 22(4): 289-295 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GJSD201304006.htm

Li, Q.W., Zhang, B., Zhang, H.H., et al., 2010.A New Understanding of Metallogenic Regularity of the Tadong Iron Deposit.Jilin Geology, 29(4):59-61 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-JLDZ201004014.htm

Liu, Y.S., Hu, Z.C., Gao, S., et al., 2008.In Situ Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS without Applying an Internal Standard.Chemical Geology, 257(1-2):34-43.doi: 10.1016/j.chemgeo.2008.08.004

Liu, Y., Gao, S., Hu, Z., et al., 2010.Continental and Oceanic Crust Recycling-Induced Melt-Peridotite Interactions in the Trans-North China Orogen:U-Pb Dating, Hf Isotopes and Trace Elements in Zircons of Mantle Xenoliths.Journal of Petrology, 51(1-2):537-571.doi: 10.1093/petrology/egp082

Ludwig, K.R., 2003.ISOPLOT 3.00:A Geochronological Toolkit for Microsoft Excel.Berkeley Geochronology Center, Berkeley. https://www.researchgate.net/publication/306157481_Isoplot_v_30_a_geochronological_toolkit_for_Microsoft_Excel

Li, D.J., Wan, Q.H., Xu, L.J., et al., 1997.Petrology and Stratum of Jilin Province.China University of Geoscience Press, Wuhan, 10-11 (in Chinese).

Peng, Y.J., Wang, Z.F., 1995.Determination of A-type Granite Zone in the Central Part of Jilin Province and Its Significance in Tectonics.Jilin Geology, 14(3):31-43 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-JLDZ503.002.htm

Peng, Y.J., Zhao, C.B., 2001.The Evolution of the Paleo Jihei Orogenic Belt and Accretion of Continental Crust.Jilin Geology, 20(2):1-9 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-JLDZ200102000.htm

Rubatto, D., Gebauer, D., 2000.Use of Cathodoluminescence for U-Pb Zircon Dating by ION Microprobe:Some Examples from the Western Alps.Cathodoluminescence in Geoscience, Springer-Verlag Berlin Heidelberg, New York, 373-400. https://www.researchgate.net/publication/230814801_Use_of_Cathodoluminescence_for_U-Pb_Zircon_Dating_by_Ion_Microprobe_Some_Examples_from_the_Western_Alps

Rubatto, D., Hermann, J., 2003.Zircon Formation During Fluid Circulation in Eclcgites (Monviso, Western Alps):Implications for Zr and Hf Budget in Subduction Zones.Geochimica et Cosmochimica Acta, 67(12):2173-2187.doi: 10.1016/S0016-7037(02)01321-2

Rubatto, D., 2002.Zircon Trace Element Geochemistry:Partitioning with Garnet and the Link between U-Pb Ages and Metamorphism.Chemical Geology, 84(1-2):123-138.doi: 10.1016/S0009-2541(01)00355-2

Shao, J.B., Zhang, X.Y., Wang, H.T., et al., 2014.Geochemistry and Pyrite Re-Os Dating of the Tadong Iron Deposit in Jilin Province.Acta Geologoca Sinica, 88(1):83-98 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE201401008.htm

Sinha, A.K., Wayne, D.M., Hewitt, D.A., 1992.The Hydrothermal Stability of Zircon:Preliminary Experimental and Isotopic Studies.Geochimica et Cosmochimica Acta, 56(9):3551-3560.doi: 10.1016/0016-7037(92)90398-3

Wang, F., Xu, W.L., Gao, F.H., et al., 2014.Precambrian Terrane within the Songnen-Zhangguangcai Range Massif, NE China:Evidence from U-Pb Ages of Detrital Zircons from the Dongfengshan and Tadong Groups.Gondwana Research, 26(1):402-413.doi: 10.1016/j.gr.2013.06017

Watson, E.B., Cherniak, D.J., Hanchar, J.M., et al., 1997.The Incorporation of Pb into Zircon.Chemical Geology, 141:19-31.doi: 10.1016/S0009-2541(97)00054-5

Wiedenbeck, M., Alle, P., Corfu, F., et al., 1995.Three Natural Zircon Standards for U-Th-Pb, Lu-Hf, Trace Element and REE Analyses.Geostandards and Geoanalytical Research, 19(1):1-23.doi: 10.1111/j.1751-908X.1995.tb00147.x

Wu, Y.B., Zheng, Y.F., 2004.Genesis of Zircons and Its Constraints on Interpretation of U-Pb Age.Chinese Science Bulletin, 49(15):1554-1569 (in Chinese). doi: 10.1007/BF03184122

Yu, J.J., Hou, X.G., Ge, W.C., et al., 2013.Magma Mixing Genesis of the Early Permian Liulian Pluton at the Northeastern Margin of the Jiamusi Massif in NE China:Evidences from Petrography, Geochronology and Geochemistry.Acta Petrologica Sinica, 29(9):2971-2986 (in Chinese with English abstract). https://www.researchgate.net/publication/282383157_Magma_mixing_genesis_of_the_Early_Permian_Liulian_pluton_at_the_northeastern_margin_of_the_Jiamusi_massif_in_NE_China_Evidences_from_petrography_geochronology_and_geochemistry

Zhang, Y.J., Sun, F.Y., Xu, C.H., et al., 2016.Geochronology, Geochemistry and Zircon Hf Isotopes of the Tanjianshan Granite Porphyry Intrusion in Dachaidan Area of the North Margin of Qaidam Basin, NW China.Earth Science, 41(11):1830-1844 (in Chinese with English abstract). https://www.researchgate.net/profile/Huaikun_Li/citations?sorting=recent&page=1

Zhang, Y.Q., 2012.Study on the Laser-Raman Spectroscopy Analysis and CL Images:Implications for Metamictized Zircons and U-Pb Ages.Geological Survey and Research, 35(3):224-228 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-QHWJ201203013.htm

寇林林, 张森, 吕俊超, 等, 2013.吉林塔东铁矿赋矿建造地球化学特征及其地质构造意义.地质与资源, 22(4): 289-295. http://www.cnki.com.cn/Article/CJFDTOTAL-GJSD201304006.htm

李东津, 万清海, 许良久等, 1997.吉林省岩石地层.武汉:中国地质大学出版社, 10-11.

李庆武, 张斌, 张红红, 等, 2010.塔东铁矿床成矿规律新认识.吉林地质, 29(4): 59-61. http://www.cnki.com.cn/Article/CJFDTOTAL-JLDZ201004014.htm

彭玉鲸, 王占福, 1995.吉林省中部A型花岗岩带的确定及其构造意义.吉林地质, 14(3): 31-43. http://www.cnki.com.cn/Article/CJFDTOTAL-JLDZ503.002.htm

彭玉鲸, 赵成弼, 2001.古吉黑造山带的演化与陆壳的增生.吉林地质, 20(2): 1-9. http://www.cnki.com.cn/Article/CJFDTOTAL-JLDZ200102000.htm

邵建波, 张希友, 王洪涛, 等, 2014.吉林省塔东大型铁矿地球化学特征及黄铁矿Re-Os同位素定年.地质学报, 88(1): 83-98. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201401008.htm

吴元保, 郑永飞, 2004.锆石成因矿物学研究及其对U-Pb年龄解释的制约.科学通报, 49(16): 1589-1604. doi: 10.3321/j.issn:0023-074X.2004.16.002

张延军, 孙丰月, 许成瀚, 等, 2016.柴北缘大柴旦滩间山花岗斑岩体锆石U-Pb年代学、地球化学及Hf同位素.地球科学, 41(11): 1830-1844. http://www.earth-science.net/WebPage/Article.aspx?id=3382

张永清, 2012.激光拉曼、阴极荧光研究对蜕晶化锆石及其U-Pb年龄解释的指示意义.地质调查与研究, 35(3): 224-228. http://www.cnki.com.cn/Article/CJFDTOTAL-QHWJ201203013.htm

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U-Pb Dating and Trance Elements Composition of Tadong Group from Jilin Province and Their Geological Implications

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