碎屑锆石U-Pb年龄谱系对兴安地块落马湖群原岩形成时代的约束

赵院冬; 车继英; 许逢明; 魏明辉

doi:10.3799/dqkx.2018.367

Volume 45 Issue 2

Feb. 2020

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Article Navigation > Earth Science > 2020 > 45(2): 489-502

Zhao Yuandong, Che Jiying, Xu Fengming, Wei Minghui, 2020. Constraints on the Forming Age of the Luomahu Group in the Xing'an Block from the Detrital Zircon Population. Earth Science, 45(2): 489-502. doi: 10.3799/dqkx.2018.367

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Zhao Yuandong, Che Jiying, Xu Fengming, Wei Minghui, 2020. Constraints on the Forming Age of the Luomahu Group in the Xing'an Block from the Detrital Zircon Population. Earth Science, 45(2): 489-502. doi: 10.3799/dqkx.2018.367

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Constraints on the Forming Age of the Luomahu Group in the Xing'an Block from the Detrital Zircon Population

doi: 10.3799/dqkx.2018.367

Shenyang Geological Survey, CGS, Shenyang 110034, China

Received Date: 2018-12-29
Publish Date: 2020-02-15

Abstract

Abstract

The series of metamorphic rocks outcropped in the Great Xing'an Range area such as Xinghuadukou Group and Luomahu Group have been considered as the metamorphic basement of the Erguna massif and Xing'an block in the eastern part of the Central Asian Orogenic Belt, but there is a great controversy over the age of its formation, which restricts the study of the regional tectonic evolution. In order to ascertain the protolith age of the Luomahu Group in the northeast of Xing' an block, this paper selects two mica schists to carry out the study of LA-ICP-MS U-Pb age of detrital zircon, and analyzes the characteristics of the provenances and the maximum sedimentary limit. The results show that the dated detrital zircons from two samples are the magmatic origin zircons, and have similar age population, which concentrated in 7 intervals as 400-430 Ma, 430-465 Ma, 470-520 Ma, 630-715 Ma, 750-830 Ma, 880-940 Ma and 1 720-1 870 Ma mainly. Combined the regional geological composition, the detrital zircon population reflects that the provenance was complex and had large space time range, but the early Paleozoic magmatic rocks from adjacent area were the main provenance, and the Proterozoic magmatic rocks and metamorphic rocks from the Erguna massif maybe another important source. Based on the minimum age of detrital zircon, it could be determined that the upper limit of sedimentary age of the protolith was Early Devonian, rather than from the Neoproterozoic to Early Cambrian as originally thought. According to the comparison of the sedimentary formation, it is inferred that the Luomahu Group may be deposited contemporaneously with the Upper Silurian-Lower Devonian series (such as the Woduhe Formation and the Niqiuhe Formation) at the same tectonic environment, and the existing differences may be caused by experiencing different metamorphisms at the later stages. The deformation and metamorphism might be related to the closure of the Mongol-Okhotsk Ocean during the Mesozoic.
- Xing'an block,
- Luomahu group,
- detrital zircon,
- the forming age,
- geochemistry

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References

Biao, S.H., Zheng, W.Z., Zhou, X.F., 2012. Zircon U-Pb Age of the North Da Hinggan Mts., NE China and Its Constraint to Attribute of the Ergun Block. Acta Geological Sinica, 86(8):1262-1272 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb201208009

Cui, F. H., Zheng, C. Q., Xu, X. C., et al., 2015. Detrital Zircon Ages of the Jiageda and Woduhe Formations: Constrains on the Tectonic Attribute of the Xing' an Terrane in the Central Great Xing' an Range, NE China. Journal of Asian Earth Sciences, 113: 427-442. doi: 10.1016/j.jseaes.2015.01.017

Dong, S.W., Zhang, Y.Q., Chen, X.H., et al., 2008. The Formation and Deformational Characteristics of East Asia Multi-Direction Convergent Tectonic System in the Late Jurassic. Acta Geoscientica Sinica, 29(3): 306-317(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqxb200803005

Dong, S. W., Zhang, Y. Q., Zhang, F. Q., et al., 2015. Late Jurassic-Early Cretaceous Continental Convergence and Intracontinental Orogenesis in East Asia: A Synthesis of the Yanshan Revolution. Journal of Asian Earth Sciences, 114: 750-770. https://doi.org/10.1016/j.jseaes.2015.08.011

Donskaya, T. V., Gladkochub, D. P., Mazukabzov, A. M., et al., 2013. Late Paleozoic-Mesozoic Subduction-Related Magmatism at the Southern Margin of the Siberian Continent and the 150 Million-Year History of the Mongol-Okhotsk Ocean. Journal of Asian Earth Sciences, 62: 79-97. https://doi.org/10.1016/j.jseaes.2012.07.023

Feng, J.X., 2006. Ore Matter Source for the Guliku Hardrock Gold Deoposit in Daxing'anling, Heilongjiang. Mineral Resources and Geology, 20(1): 54-61(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-KCYD200601010.htm

Feng, Z. Q., Liu, Y. J., Li, Y. R., et al., 2017. Ages, Geochemistry and Tectonic Implications of the Cambrian Igneous Rocks in the Northern Great Xing'an Range, NE China. Journal of Asian Earth Sciences, 144: 5-21. doi: 10.1016/j.jseaes.2016.12.006

Feng, Z.Q., Liu, Y.J., Wu, P., et al., 2018. Silurian Magmatismon the Eastern Margin of the Erguna Block, NE China: Evolution of the Northern Great Xing'an Range. Gondwana Research, 61: 46-62. doi: 10.1016/j.gr.2018.04.011

Fu, J.Y., Yu, R.G., Song, Y.Q., et al., 2005. Geological Characteristics of the Hongyejia Thrust Shear Zone Northwest of Heihe in the Heilongjiang River Valley and Its Significance. Journal of Geomechanics, 11(2):145-153(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlxxb200502006

Gao, R.Z., Xue, C.J., Lv, X.B., et al., 2017. Genesis of the Zhengguang Gold Deposit in the Duobaoshan Ore Field, Heilongjiang Province, NE China: Constraints from Geology, Geochronology and S-Pb Isotopic Compositions. Ore Geology Reviews, 84: 202-217. doi: 10.1016/j.oregeorev.2016.12.031

Ge, W.C., Wu, F.Y., Zhou, C.Y., et al., 2005. The Ages of the Tahe Granite in Northern Daxinganling and Its Implication to the Geotectonics of Ergun Terrane. Chinese Science Bulletin, 50(12):1239-1247 (in Chinese). doi: 10.1360/csb2005-50-12-1239

Ge, W.C., Wu, F.Y., Zhou, C.Y., et al., 2007a. Porphyry Cu-Mo Deposits in the Eastern Xing'an-Mongolian Orogenic Belt: Mineralization Ages and Their Geodynamic Implications. Chinese Science Bulletin, 52(20):2407- 2417(in Chinese). doi: 10.1360/csb2007-52-20-2407

Ge, W.C., Sui, Z.M., Wu, F.Y., et al., 2007b. Zircon U-Pb ages, Hf Isotopic Characteristics and Their Implications of the Early Paleozoic Granites in the Northeastern Da Hinggan Mts, Northeastern China. Acta Petrologica Sinica, 23(2): 423-440 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200702021

Ge, W.C., Chen, J.S., Yang, H., et al., 2015. Tectonic Implications of New Zircon U-Pb ages for the Xinghuadukou Complex, Erguna Massif, Northern Great Xing'an Range, NE China. Journal of Asian Earth Sciences, 106:169-185. doi: 10.1016/j.jseaes.2015.03.011

Guo, Y.F., Yang, Y.C., Han, S.J., et al., 2016. Geochemistry and Zircon U Pb Dating of the Tonalite from Fenghuangshan Areain Daxing'anling. Journal of JiLin University (Earth Science Edtion), 46(5): 1406-1417. (in Chinese with English abstract).

Han, G. Q., Liu, Y. J., Neubauer, F., et al., 2011. Origin of Terranes in the Eastern Central Asian Orogenic Belt, NE China: U-Pb Ages of Detrital Zircons from Ordovician-Devonian Sandstones, North Da Xing'an Mts.. Tectonophysics, 511(3/4): 109-124. https://doi.org/10.1016/j.tecto.2011.09.002

Hao, Y.J., Ren, Y.S., Duan, M.X., et al., 2015. Metallogenic Events and Tectonic Setting of the Duobaoshan Ore Field in Heilongjiang Province, NE China. Journal of Asian Earth Sciences, 97: 442-458. doi: 10.1016/j.jseaes.2014.08.007

Hou, K.J., Li, Y.H., Tian, Y.R., 2009. In Situ U-Pb Zircon Datingusing Laser Ablation-Multion Counting-ICP-MS. Mineral Deposits, (4):481-492 (in Chinese with English abstract) http://en.cnki.com.cn/Article_en/CJFDTOTAL-KCDZ200904009.htm

Hou, W., Liu, Z.J., He, Y.P., et al., 2010. Sedimentary Characteristics and Tectonic Setting of the Upper Jurassic Mohe Basin. Journal of Jilin University(Earth Science Edition), 40(2):286-297(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cckjdxxb201002008

Huang, Y.W., Liu, Y., Wang, X.C., et al., 2009. Petrological Features and Tectonic Significance of the Ordovician in Duobaoshan Ore District, Northern Heilongjiang. Chinese Journal of Geology, 44(1):245-256 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzkx200901019

Lei, W.Y., Shi, G.H., Liu, Y.X., 2013. Research Progress on Trace Element Characteristics of Zircons of Different Origins. Earch Science Frontiers, 20(4):273-284 http://d.old.wanfangdata.com.cn/Periodical/dxqy201304023

Li, J.Y., Mo, S.M., He, Z.J., et al., 2004. The Timing of Crustal Sinistral Strike-Slip Movement in the Northern Great Khing'an Ranges and Its Constraint on Reconstruction of the Crustal Tectonic Evolution of NE China and Adjacent Areas Since the Mesozoic. Earth Science Frontiers, 11(3):157-168. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy200403017

Liu, J., Li, Y., Zhou, Z.H., et al., 2017. The Ordovician Igneous Rocks with High Sr/Y at the Tongshan Porphyry Copper Deposit, Satellite Of the Duobaoshan Deposit, and their Metallogenic Role. Ore Geology Reviews, 86: 600-614. doi: 10.1016/j.oregeorev.2017.02.036

Liu, Y.J., Li, W.M., Feng, Z.Q., et al., 2017. A Review of the Paleozoic Tectonics in the Eastern Part of Central Asian Orogenic Belt. Gondwana Research, 43: 123-148. doi: 10.1016/j.gr.2016.03.013

Lu, S.N., Chen, Z.H., Xiang, Z.Q., et al., 2006. U-Pb Ages of Detrital Zircons From the Parametamorphic Rocks of the Qinling Group and Their Geological Significance. Earth Science Frontiers, 13(6):303-310(in Chinese with English abstract).

Miao, L.C., Fan, W.M., Zhang, F.Q., et al., 2003. Zircon SHRIMP Geochronology of the Xinkailing-Kele Complex in the Northwestern Lesser Xing'an Range, and Its Geological Implications. Chinese Science Bulletin, 49: 2201-2209 (in Chinese).

Miao, L.C., Liu, D.Y., Zhang, F.Q., et al., 2007. Zircon SHRIMP U-Pb Ages of the "Xinghuadukou Group" in Hanjiayuanzi and Xinlin Areas and the "Zhanlantun Group"in Inner Mongolia, Great Xing'an Range.Chinese Science Bulletin, 52(5):591-601 (in Chinese). doi: 10.1360/csb2007-52-5-591

Miao, L.C., Zheng, F.Q., Zhu, M.S., et al., 2015. Zircon SHRIMP U-Pb Dating of Metamorphic Complexes in the Conjunction of the Greater and Lesser Xing'an Ranges, NE China: Timing of Formation and Metamorphism and Tectonic Implications. Journal of Asian Earth Sciences, 114: 634-648. doi: 10.1016/j.jseaes.2014.09.035

Nelson, D.R., 2001. An Assessment of the Determination of Depositional Ages for Precambrian Clastic Sedimentary Rock By U-Pb Dating of Detrital Zircon. Geological Society of America Bulletin, 141/142:137-160. http://www.sciencedirect.com/science/article/pii/S0037073801000677

Qi, Z.Y., Feng, Z.Q., Wen, Q.B. et al., 2017. Petrogenesis of the Early Paleozoic Diorite in the Northeast Nenjiang Area: Evidence from Zircon U-Pb Chronology and Geochemistry. Journal of Jilin University (Earth Science Edition), 47(1):113-125 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-CCDZ201701011.htm

Shao, J., Li, Y.F., Zhou, Y.H., et al., 2015. Neo-Achaean Magmatic Event in Erguna Massif of Northeast China: Evidence from the Zircon LA-ICP-MS Dating of the Gneissic Monzogranite from the Drill. Journal of Jilin University: Earth Science Edition, 45(2):364-373 (in Chinese with English abstract).

She, H.Q., Li, J.W., Xiang, A.P., et al., 2012. U-Pb Ages of the Zircons from Primary Rocks in Middle-Northern Daxinganling and its Implications to Geotectonic Evolution. Acta Petrologica Sinica, 28(2):571- 594 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201202018

Song, G.X., Qin, K.Z., Wang, L., et al., 2015. Type, Zircon U-Pb Age and Paleovolcano Edifice of Zhengguang Gold Deposit in Duobaoshan Orefield in Heilongjiang Province, NE-China. Acta Petrologica Sinica, 31(8):2402- 2416(in Chinese with English abstract).

Sui, Z.M., Ge, W.C., Wu, F.Y., et al., 2006. U-Pb Chronology in Zircon from Harabaqi Granitic Pluton in Northern Daxinganling Area and Its Origin. Global Geology, 23(3):229-236 (in Chinese with English abstract).

Sun, L.X., Ren, B.F., Zhao, F.Q., et al., 2013. Late Paleoproterozoic Magmatic Records in the Erguna Massif: Evidences from the Zircon U-Pb Dating of Granitic Gneisses. Geological Bulletin of China, 32(2-3):341-352(in Chinese with English abstract).

Sun, W. 2014. Zircon Geochronology Constraints on the Age and Nature of "Precambrian Metamorphic Rocks" and Lower Paleozoicin the Xing'an Block of Northeast China(Dissertation). Jilin University, Changchun (in Chinese with English abstract).

Tan, C.Y., Du, Y.S., Zhao, H.D., et al., 2009. The NW-Trending Tectonic-Metallogenic Belt of Nonferrous and Precious Metals on the Right of the Heilongjiang River and its Geological Implication. Geology and Resources, 18(4): 256-266(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gjsdz200904004

Tang, J., Xu, W.L., Wang, F., et al., 2013. Geochronology and Geochemistry of Neoproterozoic Magmatism in the Erguna Massif, NE China: Petrogenesis and Implications for the Breakup of the Rodinia Supercontinent. Precambrian Research, 224: 597-611. doi: 10.1016/j.precamres.2012.10.019

Wang, L., Qin, K.Z., Song, G.X., et al., 2018. Volcanic-Subvolcanic Rocks and Tectonic Setting of the Zhengguang Intermediate Suffixation Epithermal Au-Zn Deposit, Eastern Central Asian Orogenic Belt, ChinaNE. Journal of Asian Earth Sciences. https://doi.org/ https://doi.org/10.1016/j.jseaes.2018.07.023

Wu, F.Y., Sun, D.Y., Ge, W.C., et al., 2011. Geochronology of the Phanerozoic Granitoids in Northeastern China. Journal of Asian Earth Sciences, 41(1):1-30. doi: 10.1016/j.jseaes.2010.11.014

Wu, G., 2005. Metallogenic Setting and Metallogenesis of Nonferrous-Precious Metals in Northern Da Hinggan Moutain(Dissertation). Jilin University, Changchun (in Chinese with English abstract).

Wu, G., Chen, Y.J., Sun, F.Y., et al., 2008. Geochemistry of the Late Jurassic Granitoids in the Northern End Area of Da Hinggan Mountains and Their Geological and Prospecting implications. Acta Petrologica Sinica, 24(4):899-910. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200804028

Wu, G., Chen, Y.C., Chen, Y.J., et al., 2012. Zircon U-Pb ages of the Metamorphic Supracrustal Rocks of the Xinghuadukou Group and Granitic Complexes in the Argun Massif of the Northern Great Hinggan Range, NE China, and Their Tectonic Implications. Journal of Asian Earth Sciences, 49: 214-233. doi: 10.1016/j.jseaes.2011.11.023

Wu, Y.B., Zheng, Y.F., 2004. Zircon Genetic Mineralogy and its Constraints on U-Pb Age Interpretation. Chinese Science Bulletin, 49(16): 1589-1604(in Chinese). doi: 10.1360/csb2004-49-16-1589

Wu, G.Y., Feng, Z.Q., Yang, J.G., et al., 2006. Tectonic Setting and Geological Evolution of Mohe Basin in Northwest China. Oil and Gas Geology, 27(4):528-535(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYYT200604014.htm

Xiang, A.P., Yang, Y.C., Li, G.T., et al., 2012. Diagenetic and Metallogenic Ages of Duobaoshan Porphyry Cu- Mo Deposit in Heilongjiang Province. Mineral Deposits, 31(6):1237-1248 (in Chinese). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kcdz201206009

Xu, B., Zhao, P., Wang, Y.Y., et al., 2015. The Pre-Devonian Tectonic Framework of Xing'an-Mongolia Orogenic Belt (XMOB) in North China. Journal of Asian Earth Sciences, 97: 183-196. doi: 10.1016/j.jseaes.2014.07.020

Yang, X.L., 2007. Geological Characteristics and Study of Detrital Zircon Geochronology of Epimetamorphic Rock Series in Zhalantun Area(Dissertation). Jilin University, Changchun (in Chinese with English abstract).

Zeng, Q.D., Liu, J.M., Chu, S.X., et al., 2014. Re-Os and U-Pb Geochronology of the Duobaoshan Porphyry Cu-Mo-(Au) Deposit, Northeast China, and Its Geological Significance. Journal of Asian Earth Sciences, 79: 895-909. doi: 10.1016/j.jseaes.2013.02.007

Zhao, H.B., Mo, X.X., Xu, S.M. et al., 2007. Composition and Evolution of the Xinlailing Metamorphic Core Complexes in Heilongjiang Province. Chinese Journal of Geology, 42(1):176-188(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKX200701018.htm

Zhao, Y.D., Mo, X.X., Li, S.C., et al., 2015. Zircon U-Pb LA-ICP-MS Dating, Petro-Geochemical Features of Granitic Mylonite in Northwestern Lesser Hinggan Mountains, and Tectonic Significance. Geological Review, 61: 443-457 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DZLP201502022.htm

Zhao, Y.D, Xu, F.M., Che, J.Y., et al., 2017a. Constraints from the Zircon U-Pb Dating on the Formation Age and Composition of the Xinhuadukou Group in Northeastern Da Hinggan Mountains. Geology in China, 44(3):575- 587(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi201703013

Zhao, Y.D., Che, J.Y., Wu, D.T., et al., 2017b. Early-Middle Jurassic TTG Granites in Northwest of Lessor Xing'an Range: Its Geochronology, Geochemical Characteristics and Tectonic Significance. Journal of Jinlin University(Earth Science Edition), 47(4):1119-1137(in Chinese with English abstract).

Zhou, J.B., Zhang, X.Z., Wilde, A.S., et al., 2011a. Confirming of the Heilongjiang ~500 Ma Pan-African Khondalite Belt and its Tectonic Implications. Acta Petrologica Sinica, 27(4):1235-1245. http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201104031.htm

Zhou, J.B., Wilde, S.A., Zhang, X.Z., et al., 2011b. Early Paleozoic Metamorphic Rocks of the Erguna Block in the Great Xing'an Range, NE China: Evidence for the Timing of Magmatic and Metamorphic Events and Their Tectonic Implications. Tectonophysics, 499(1-4): 105-117. doi: 10.1016/j.tecto.2010.12.009

Zhou, J.B., Wang, B., Zeng, W.S., et al., 2014. Detrital Zircon U-Pb Dating of the Zhalantun Metamorphic Complex and Its Tectonic Implications, Great Xing'an, NE China. Acta Petrologica Sinica, 30(7):1879-1888 (in Chinese with English abstract) http://d.old.wanfangdata.com.cn/Periodical/ysxb98201407004

Zhou, J.B., Wang, B., Wilde, S.A., et al., 2015. Geochemistry and U-Pb Zircon Dating of the Toudaoqiao Blueschists in the Great Xing'an Range, Northeast China, and Tectonic Implications. Journal of Asian Earth Sciences, 97: 197-210. doi: 10.1016/j.jseaes.2014.07.011

表尚虎, 郑卫政, 周兴福, 2012.大兴安岭北部锆石U_Pb年龄对额尔古纳地块构造归属的制约.地质学报, 86(8): 1262-1272. doi: 10.3969/j.issn.0001-5717.2012.08.009

董树文, 张岳桥, 陈宣华, 等, 2008.晚侏罗世东亚多向汇聚构造体系的形成与变形特征.地球学报, 29(3): 306-317. doi: 10.3321/j.issn:1006-3021.2008.03.005

冯健行, 2006.黑龙江省大兴安岭古利库岩金矿床成矿物质来源分析.矿产与地质, 20(1): 54-61. doi: 10.3969/j.issn.1001-5663.2006.01.011

付俊彧, 于荣文, 宋亚芹, 等, 2005.黑龙江黑河西北洪业家推覆剪切构造带地质特征及其意义.地质力学学报, 11(2):145-153. doi: 10.3969/j.issn.1006-6616.2005.02.006

葛文春, 吴福元, 周长勇, 等. 2005.大兴安岭北部塔河花岗岩体的时代及对额尔古纳地块构造归属的制约.科学通报, 50(12):1239-1247. doi: 10.3321/j.issn:0023-074X.2005.12.015

葛文春, 吴福元, 周长勇, 等, 2007a.兴蒙造山带东段斑岩型Cu-Mo矿床成矿时代及其地球动力学意义[J].科学通报, 52(20):2407-2417. http://www.cnki.com.cn/Article/CJFDTotal-KXTB200720014.htm

葛文春, 隋振民, 吴福元, 等, 2007b.大兴安岭东北部早古生代花岗岩锆石U-Pb年龄、Hf同位素特征及地质意义.岩石学报, 23(2):423-440. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200702021

郭宇飞, 杨言辰, 韩世炯, 等, 2016.大兴安岭北部凤凰山地区英云闪长岩地球化学特征与锆石U-Pb定年.吉林大学学报(地球科学版), 46(5): 1406-1417. http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb201605012

侯可军, 李延河, 田有荣, 2009. LA-MC-ICP-MS锆石微区原位U-Pb定年技术.矿床地质, 28(4):481-492. doi: 10.3969/j.issn.0258-7106.2009.04.010

侯伟, 刘昭君, 何玉平, 等, 2010.漠河盆地上侏罗统沉积特征与构造背景.吉林大学学报(地球科学版), 40(2):286-297. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cckjdxxb201002008

黄永卫, 刘扬, 王喜臣, 等, 2009.黑龙江北部多宝山矿区奥陶系的岩石特征和构造意义.地质科学, 44(1): 245-256. doi: 10.3321/j.issn:0563-5020.2009.01.019

雷玮琰, 施光海, 刘迎新, 2013.不同成因锆石的微量元素特征研究进展.地学前缘, 20(4): 273-284. http://d.old.wanfangdata.com.cn/Periodical/dxqy201304023

李锦轶, 莫申国, 和政军, 等, 2004.大兴安岭北段地壳左行走滑运动的时代及其对中国东北及邻区中生代以来地壳构造演.地学前缘, 11(3):157-168. doi: 10.3321/j.issn:1005-2321.2004.03.017

陆松年, 陈志宏, 相振群, 等, 2006.秦岭岩群副变质岩碎屑锆石年龄谱及其地质意义探讨.地学前缘, 13(6): 303-310. doi: 10.3321/j.issn:1005-2321.2006.06.033

苗来成, 范蔚茗, 张福勤, 等. 2003.小兴安岭西北部新开岭-科洛杂岩锆石SHRIMP年代学研究及其意义.科学通报, 48: 2315-2323. doi: 10.3321/j.issn:0023-074X.2003.22.004

苗来成, 刘敦一, 张福勤, 等, 2007.大兴安岭韩家园子和新林地区兴华渡口群和扎兰屯群锆石SHRIMP U-Pb年龄.科学通报, 52(5): 591-602. doi: 10.3321/j.issn:0023-074X.2007.05.016

齐忠友, 冯志强, 温泉波, 等, 2017.东北地区嫩江东北部早古生代闪长岩的成因探讨:锆石U-Pb年代学和地球化学证据.吉林大学学报(地球科学版), 47(1): 113-125. http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb201701011

邵军, 李永飞, 周永恒, 等, 2015.中国东北额尔古纳地块新太古代岩浆事件-钻孔片麻状二长花岗岩锆石LA-ICP-MS测年证据.吉林大学学报(地球科学版), 45(2): 364-372. http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb201502004

佘宏全, 李进文, 向安平, 等, 2012.大兴安岭中北段原岩锆石U-Pb测年及其与区域构造演化关系.岩石学报, 28(2): 571-594. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201202018

宋国学, 秦克章, 王乐, 等, 2015.黑龙江多宝山矿田争光金矿床类型U-Pb年代学及古火山机构.岩石学报, 31(8): 2402-2416. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201508019

宋鹰, 钱禛钰, 张俊霞, 等, 2018.碎屑锆石形态学分类体系及其在物源分析中的应用:以松辽盆地松科一井为例.地球科学, 43(6):1997-2006. doi: 10.3799/dqkx.2018.607

隋振民, 葛文春, 吴福元, 等, 2006.大兴安岭东北部哈拉巴奇花岗岩体锆石U-Pb年龄及其成因.世界地质, 23(3):229-236. doi: 10.3969/j.issn.1004-5589.2006.03.003

孙立新, 任邦方, 赵凤清, 等, 2013.内蒙古额尔古纳地块古元古代末期的岩浆记录-来自花岗片麻岩的锆石U-Pb年龄证据.地质通报, 32(2/3): 341-352. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz201302013

孙巍. 2014.兴安地块"前寒武纪变质岩系"——下古生界锆石年代学研究及其构造意义(博士学位论文).长春: 吉林大学.

谭成印, 杜杨松, 赵寒冬, 等, 2009.黑龙江右岸北西向有色、贵金属构造-成矿带的确立及其地质意义.地质与资源, 18(4): 256-266. doi: 10.3969/j.issn.1671-1947.2009.04.004

王照元, 郑常青, 徐久磊, 等, 2018.内蒙古莫尔道嘎佳疙瘩组变质岩地球化学特征及构造意义.地球科学, 43(1):176-198 doi: 10.3799/dqkx.2018.011

武广, 2005.大兴安岭北部区域成矿背景与有色-贵金属矿床成矿作用(博士学位论文).长春: 吉林大学.

武广, 陈衍景, 孙丰月, 等, 2008.大兴安岭北端晚侏罗世花岗岩类地球化学及其地质和找矿意义.岩石学报, 24(4):899-910. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200804028

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

吴根耀, 冯志强, 杨建国, 等, 2006.中国东北漠河盆地的构造背景和地质演化.石油与天然气地质, 27(4):528-535. doi: 10.3321/j.issn:0253-9985.2006.04.014

向安平, 杨郧城, 李贵涛, 等, 2012.黑龙江多宝山斑岩Cu-Mo矿床成岩成矿时代研究.矿床地质, 31(6): 1237-1248. doi: 10.3969/j.issn.0258-7106.2012.06.009

杨现力. 2007.扎兰屯浅变质岩系地质特征及碎屑锆石年代学研究(硕士学位论文).长春: 吉林大学.

赵海滨, 莫宣学, 徐受民, 等, 2007.黑龙江新开岭变质核杂岩的组成及其演化.地质科学, 42(1):176-188. doi: 10.3321/j.issn:0563-5020.2007.01.015

赵院冬, 莫宣学, 李士超, 等, 2015.小兴安岭西北部花岗质糜棱岩锆石LA-ICP-MS+U-Pb年龄、岩石地球化学特征及地质意义.地质论评, 61(2): 443-457. http://d.old.wanfangdata.com.cn/Periodical/dzlp201502017

赵院冬, 许逢明, 车继英, 等, 2017a.锆石U-Pb定年对大兴安岭东北部"兴华渡口群"形成时代和组成的约束.中国地质, 44(3): 575-587. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi201703013

赵院冬, 车继英, 吴大天, 等, 2017b.小兴安岭西北部早-中侏罗世TTG花岗岩年代学、地球化学特征及构造意义.吉林大学学报(地球科学版), 47(4):1119-1137. http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb201704012

周建波, 张兴洲, WILDE, S.A., 等, 2011.中国东北~500 Ma泛非期孔兹岩带的确定及其意义.岩石学报, 27(4): 1235-1245.

周建波, 王斌, 曾维顺, 等, 2014.大兴安岭地区扎兰屯变质杂岩的碎屑锆石U-Pb年龄及其大地构造意义.岩石学报, 30(7): 1879-1888. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201407004

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