华北克拉通南缘约2.5 Ga构造变质事件及意义

曹正琦; 翟文建; 蒋幸福; 胡正祥; 曾佐勋; 蔡逸涛; 张雄; 徐少朋; 郭君功

doi:10.3799/dqkx.2016.047

Volume 41 Issue 4

Apr. 2016

Turn off MathJax

Article Contents

Abstract

References

Article Navigation > Earth Science > 2016 > 41(4): 570-585

Cao Zhengqi, Zhai Wenjian, Jiang Xingfu, Hu Zhengxiang, Zeng Zuoxun, Cai Yitao, Zhang Xiong, Xu Shaopeng, Guo Jungong, 2016. About 2.5 Ga Tectono-Metamorphic Event in Southern Margin of North China Craton and Its Significance. Earth Science, 41(4): 570-585. doi: 10.3799/dqkx.2016.047

Citation:

Cao Zhengqi, Zhai Wenjian, Jiang Xingfu, Hu Zhengxiang, Zeng Zuoxun, Cai Yitao, Zhang Xiong, Xu Shaopeng, Guo Jungong, 2016. About 2.5 Ga Tectono-Metamorphic Event in Southern Margin of North China Craton and Its Significance. Earth Science, 41(4): 570-585. doi: 10.3799/dqkx.2016.047

Citation:

Cao Zhengqi, Zhai Wenjian, Jiang Xingfu, Hu Zhengxiang, Zeng Zuoxun, Cai Yitao, Zhang Xiong, Xu Shaopeng, Guo Jungong, 2016. About 2.5 Ga Tectono-Metamorphic Event in Southern Margin of North China Craton and Its Significance. Earth Science, 41(4): 570-585. doi: 10.3799/dqkx.2016.047

PDF( 4373 KB)

About 2.5 Ga Tectono-Metamorphic Event in Southern Margin of North China Craton and Its Significance

doi: 10.3799/dqkx.2016.047

1.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
Hubei Geological Survey, Wuhan 430034, China
3.
Henan Institute of Geological Survey, Zhengzhou 450001, China
4.
Faculty of Earth Sciences, East China University of Technology, Nanchang 330013, China
5.
Nanjing Center, China Geological Survey, Nanjing 210016, China

Received Date: 2015-07-12
Publish Date: 2016-04-15

Abstract

Abstract

Linshan Group, located in the southern margin of the central orogenic belt of the North China Craton, is a Precambrian basement. It is important to study the collision era of the central orogenic belt and the distribution of the southern margin of the North China Craton. A study was carried out on the metabasite (plagioclase-amphibole schist) of the Linshan Group for the purpose of constraining the collisional time of the central orogenic belt and its distribution through the zircon U-Pb dating and rock geochemical methods. The results obtained show that most of zircon grains from plagioclase-amphibole schist are long columnar, euhedral to subhedral, and show typical core-rim structure with irregular shape, weak zoning, taxitic zoning and sector zoning structure. Some zircons preserve the inherited cores of the early magma. Zircon rims display characteristics of dissolution texture with low Th/U ratios (most of them less than 0.09), however, zircons' cores show typical oscillatory zoning structure and relatively high Th/U ratios ranging from 0.10 to 9.24. The evidence suggests that the zircons of plagioclase-amphibole schist could be metamorphic origin. Relict cores and rims of the zircons from the plagioclase-amphibole schist yield ages of 2 528±43 Ma (MSWD=1.5, n=10) and 2 474±22 Ma (MSWD=1.3, n=21), respectively. The former data represent residual age of protolith, and the latter indicate a circa 2.5 Ga metamorphic event in the central orogenic belt of the North China Craton. Whole-rock geochemical results show that metabasite samples from the Linshan Group have relatively low contents of SiO₂ (47.70%-50.77%, average=48.90%) and K₂O (0.56%-1.78%, average=1.13%), and are depleted in high field strength elements (eg., Nb, Th, Ti and Zr) with flat REE patterns. Moreover, the geochemical samples have low content of Zr (less than 130×10^-6) and ratios of Zr/Y (less than 4), indicating that the Linshan Group could have been formed in the subducted-related island arc environment. Therefore, the above evidence show that the central orogenic belt that formed by the collision orogenesis between eastern block and western block of the North China Craton experienced late Neoarchean to early Paleoproterozoic subduction-collisional event.
- early Paleoproterozoic,
- metamorphic event,
- Linshan Group,
- North China Craton,
- central orogenic belt,
- isotope,
- tectonics

FullText(HTML)

致谢: 本文部分投图是利用长江大学路远发教授开发的Geokit软件完成.衷心感谢中国地质大学(武汉)地球科学学院郑建平教授的指导意见及3位匿名评审专家提出的宝贵修改意见.

References(98)

References

Agrawal, S., Guevara, M., Verma, S.P., 2008.Tectonic Discrimination of Basic and Ultrabasic Volcanic Rocks through Log-Transformed Ratios of Immobile Trace Elements.International Geology Review, 50:1057-1079. doi: 10.2747/0020-6814.50.12.1057

Condie, K.C., 1989.Geochemical Changes in Basalts and Andesites across the Archaean-Proterizoic Boundary:Identification and Significance.Lithos, 23:1-18. doi: 10.1016/0024-4937(89)90020-0

Deng, H., Kusky, T.M., Polat, A., et al., 2013.Geochemistry of Neoarchean Mafic Volcanic Rocks and Late Mafic Dikes in the Zanhuang Complex, Central Orogenic Belt, North China Craton: Implications for Geodynamic Setting.Lithos, 175(5):193-212. http://www.sciencedirect.com/science/article/pii/S0024493713001503

Deng, H., Kusky, T.M., Polat, A., et al., 2014.Geochronology, Mantle Source Composition and Geodynamic Constraints on the Origin of Neoarchean Mafic Dikes in the Zanhuang Complex, Central Orogenic Belt, North China Craton.Lithos, 205(9):359-378. https://www.researchgate.net/profile/Hao_Deng10/publication/264123483_Geochronology_mantle_source_composition_and_geodynamic_constraints_on_the_origin_of_Neoarchean_mafic_dikes_in_the_Zanhuang_Complex_Central_Orogenic_Belt_North_China_Craton/links/5508c7e80cf26ff55f83cd4f.pdf?disableCoverPage=true

Deng, J.F., Wu, Z.X., Zhao, G.C., et al., 1999.Precambrian Granitic Rocks, Continental Crustal Evolution and Craton Formation of the North China Platform.Acta Petrologica Sinica, 15(2):190-198(in Chinese with English abstract). https://www.researchgate.net/publication/279587697_Precambrian_granitic_rocks_continental_crustal_evolution_and_craton_formation_of_the_North_China_Platform

Diwu, C.R., Sun, Y., Guo, A., et al., 2011.Crustal Growth in the North China Craton at ~2.5 Ga:Evidence from In-Situ Zircon U-Pb Ages, Hf Isotopes and Whole-Rock Geochemistry of the Dengfeng Complex.Gondwana Research, 20:149-170. http://www.cqvip.com/QK/86894X/200924/32393543.html

Farahat, E.S., 2010.Neoproterozoic Arc-Back-Arc System in the Central Eastern Desert of Egypt:Evidence from Supra-Subduction Zone Ophiolites.Lithos, 120(3-4):293-308. doi: 10.1016/j.lithos.2010.08.017

Gao, M., Gao, F., 1988.Retrogressive Metamorphism of Archaean Granulites and the Evidence of Rb-Sr Isochron Age in Zhangjiakou and Xuanhua Regions.Journal of Hebei College of Geology, 11(4):11-19(in Chinese with English abstract). https://www.researchgate.net/publication/222312152_Archean_blocks_and_their_boundaries_in_the_North_China_Craton_Lithological_geochemical_structural_and_P-T_path_constraints_and_tectonic_evolution

Gebauer, D., 1996.A P-T-t Path for a High-Pressure Ultramafic Mafic Rock-Association and Its Felsic Country-Rocks Based on SHRIMP-Dating of Magmatic and Metamorphics Zircon Domains.Example:Alps Arami Central Swiss Alps.In:Reading the lsotopic Code, Geophsical Monograph 95.Am.Geophys.Union, Washington D.C., 307-329. doi: 10.1029/GM095p0307/pdf

Gibson, I.L., Kirkpatrick, R.J., Emmerman, R., et al., 1982.The Trace Element Composition of the Lavas and Dikes from a 3 km Vertical Section through the Lava Pile of Eastern Iceland.Journal of Geophysical Research, 87:6532-6546. doi: 10.1029/JB087iB08p06532

Guan, H., Sun, M., Xu, P., 1998.Geochronological Study of Zircons from High-Grade Gneisses of Fuping Complex by LP-ICPMS Technique.Acta Petrologica Sinica, 14(4):460-470(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB804.004.htm

Guo, J.H., O'Brien, P.J., Zhai, M.G., 2002.High-Pressure Granulites in the Sanggan Area, North China Craton:Metamorphic Evolution, P-T Paths and Geotectonic Significance.Journal of Metamorphic Geology, 20:741-756. doi: 10.1046/j.1525-1314.2002.00401.x

Guo, J.H., Sun, M., Chen, F.K., et al., 2005.Sm-Nd and SHRIMP U-Pb Zircon Geochronology of High-Pressure Granulites in the Sanggan Area, North China Craton:Timing of Paleoproterozoic Continental Collision.Journal of Asian Earth Sciences, 24:629-642. doi: 10.1016/j.jseaes.2004.01.017

Guo, R.R., Zhai, M.G., Santosh, M., et al., 2013.Geochemistry, Zircon U-Pb Geochronology and Lu-Hf Isotopes of Metavolcanics from Eastern Hebei Reveal Neoarchean Subduction Tectonics in the North China Craton.Gondwana Research, 24(2):664-686. doi: 10.1016/j.gr.2012.12.025

Hu, B., Zhai, M.G., Peng, P., et al., 2013.Late Paleoproterozoic to Neoproterozoic Geological Events of the North China Craton:Evidences from LA-ICP-MS U-Pb Geochronology of Detrital Zircons from the Cambrian and Jurassic Sedimentary Rocks in Western Hills of Beijing.Acta Petrologica Sinica, 29(7):2508-2536(in Chinese with English abstract). https://www.researchgate.net/publication/286203630_Late_Paleoproterozoic_to_Neoproterozoic_geological_events_of_the_North_China_Craton_Evidences_from_LA-ICP-MS_U-Pb_geochronology_of_detrital_zircons_from_the_Cambrian_and_Jurassic_sedimentary_rocks_in_

Kelemen, P.B., Johnson, K.T.M., Kinzler, R.J., et al., 1990.High-Field-Strength Element Depletions in Arc Basalts Due to Mantle-Magma Interaction.Nature, 345:521-523. doi: 10.1038/345521a0

Kusky, T.M., 2004.Introduction.Developments in Precambrian Geology.In:Kusky, T.M., ed., Precambrian Ophiolites and Related Rocks.Elsevier, Amsterdam, 1-34. doi: 10.1029/GM095p0307/pdf

Kusky, T.M., 2011.Geophysical and Geological Tests of Tectonic Models of the North China Craton.Gondwana Research, 20:26-35. doi: 10.1016/j.gr.2011.01.004

Kusky, T.M., Li, J.H., 2003.Paleoproterozoic Tectonic Evolution of the North China Craton.Journal of Asian Earth Sciences, 22:23-40. https://www.researchgate.net/profile/Timothy_Kusky/publication/222825952_Paleoproterozoic_tectonic_evolution_of_the_North_China_Craton/links/02e7e518077df22aa8000000.pdf?inViewer=0&pdfJsDownload=0&origin=publication_detail

Kusky, T.M., Windley, B.F., Zhai, M.G., 2007.Tectonic Evolution of the North China Block:From Orogen to Craton to Orogen.In:Zhai, M.G., Windley, B.F., Kusky, T.M., et al., eds., Mesozoic Sub-Continental Lithospheric Thinning under Eastern Asia.Geological Society of London, Special Publication, 280:1-34. https://www.researchgate.net/profile/Brian_Windley/publication/235769330_Tectonic_Evolution_of_the_North_China_Block_From_Orogen_to_Craton_to_Orogen/links/0912f51362281781f2000000.pdfhttps://www.researchgate.net/profile/Brian_Windley/publication/235769330_Tectonic_evolution_of_the_North_China_Block_from_orogen_to_craton_to_orogen/links/0912f51362281781f2000000.pdf?disableCoverPage=true

Le, R., Dick, A.P., Brlank, H.J.B., et al., 1983.Geochemistry, Mineralogy and Petrogensis of Lavas Erupted along the Southwest Indian Ridge between the Bouvettriple Gunction and 11 Degree East.Journal of Petrology, 24:267-318. doi: 10.1093/petrology/24.3.267

Lei, W.Y., Shi, G.H., Liu, Y.X., 2013.Research Progress on Trace Element Characteristics of Zircons of Different Origins.Earth Science Frontiers, 20(4):273-284(in Chinese with English abstract). https://www.researchgate.net/publication/279571372_Research_progress_on_trace_element_characteristics_of_zircons_of_different_origins

Li, J., Kusky, T., 2007.A Late Archean Foreland Fold and Thrust Belt in the North China Craton:Implications for Early Collisional Tectonics.Gondwana Research, 12:47-66. doi: 10.1016/j.gr.2006.10.020

Li, J.H., Kusky, T.M., Huang, X., 2002.Archean Podiform Chromitites and Mantle Tectonites in Ophiolitic Mélange, North China Craton:A Record of Early Oceanic Mantle Processes.GSA Today, 12:4-11.doi: 10.1130/1052-5173

Li, J.H., Niu, X.L., Chen, Z., et al., 2004.Discovery of Deep-Level Foreland Thrust-Fold Structures in Taihang Mt.and Its Implication for Early Tectonic Evolution of North China.Progress in Natural Science, 14(10):1118-1127(in Chinese). http://industry.wanfangdata.com.cn/dl/Detail/Periodical?id=Periodical_zrkxjz-e200503006

Liu, D.Y., Wan, Y.S., Wu, J.S., et al., 2007.Archean Crustal Evolution and the Oldest Rocks in the North China Craton.Geological Bulletin of China, 26(9):1131-1138(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD200709016.htm

Liu, S.J., Jahn, B.M., Wan, Y.S., et al., 2014.Neoarchean to Paleoproterozoic High-Pressure Mafic Granulite from the Jiaodong Terrain, North China Craton:Petrology, Zircon Age Determination and Geological Implications.Gondwana Research, 01293:1-16. http://linkinghub.elsevier.com/retrieve/pii/S1342937X14002305

Liu, S.W., Santosh, M., Wang, W., et al., 2011.Zircon U-Pb Chronology of the Jianping Complex:Implications for the Precambrian Crustal Evolution History of the Northern Margin of North China Craton.Gondwana Research, 20:48-63. doi: 10.1016/j.gr.2011.01.003

Liu, Y.S., Gao, S., Hu, Z.C., et al., 2009.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, 51:537-571. http://www.oalib.com/references/19218164

Liu, Y.S., Hu, Z.C., Zong, K.Q., et al., 2010.Reappraisement and Refinement of Zircon U-Pb Isotope and Trace Element Analyses by LA-ICP-MS.Chinese Science Bulletin, 55:1535-1546. doi: 10.1007/s11434-010-3052-4

Liu, Z.H., Wang, A.J., Li, X.F., 1997.Metamophism Evolution of the Late Archen Collsion Orogenic Belt in Wutaishan.Geological Journal of China Universities, 3(2):162-170(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQXB502.000.htm

Luo, Z.B., Zhang, H.F., Diwu, C.R., et al., 2012.Zircon U-Pb, Lu-Hf Isotope and Trace Element Compositions of Intermediata Pyroxene Granulite in the Huai'an Area, Northwest Hebei Province:Constraints on the Timing of Retrograde Metamorphism.Acta Petrologica Sinica, 28(11):3721-3738(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201211024.htm

Pfander, J.A., Munker, C., Stracke, A., et al., 2007.Nb/Ta and Zr/Hf in Ocean Island Basalts:Implications for Crust-Mantle Differentiation and the Fate of Niobium.Earth and Planetary Science Letters, 254 (1-2):158-172. doi: 10.1016/j.epsl.2006.11.027

Polat, A., Kusky, T.M., Li, J.H., et al., 2005.Geochemistry of the Late Archean (ca.2.55-2.50 Ga) Volcanic and Ophiolitic Rocks in the Wutaishan Greenstone Belt, Central Orogenic Belt, North China Craton:Implications for Geodynamic Setting and Continental Growth.Geological Society of America Bulletin, 117:1387-1399. doi: 10.1139/e02-070?journalCode=cjes

Qi, L., Hu, J., Gregoire, D.C., 2000.Determination of Trace Elements in Granites by Inductively Coupled Plasma-Mass Spectrometry.Talanta, 51:507-513. doi: 10.1016/S0039-9140(99)00318-5

Roberta, L., Rudnick, D., Fountain, M., 1995.Nature and Composition of the Continental Crust:A Lower Crustal Perspective.Reviews of Geophysics, 3(33):267-309. doi: 10.1029/95RG01302/full?scrollTo=footer-citing

Sun, M., Guan, H., 2001.Zircon U-Pb Ages of the Fuping Complex and Their Implications:Some Comments on the Geochronological Study of the Precambrian High-Grade Metamorphic Terranes.Acta Petrologica Sinica, 17(1):145-156(in Chinese with English abstract). https://www.researchgate.net/publication/279756005_Zircon_U-Pb_ages_of_the_fuping_complex_and_their_implications_Some_comments_on_the_geochronological_study_of_the_precambrian_high-grade_metamorphic_terranes?_sg=ILPQfU5EsWRBopAc7X9beTZNLvd_EMpjWXSOyBm-4fffitXxfgmUEgZ0k3rq5hCWpirO8IyfVprdGe0TlkUOAI67Q5Hja2dI1MEGiE9qDHc

Sun, S.S., McDonough, M.C., 1989.Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes.Geological Society Special Publication, 42:313-345. doi: 10.1144/GSL.SP.1989.042.01.19

Wan, Y.S., Miao, P.S., Liu, D.Y., et al., 2010.Formation Ages and Source Regions of the Palaeoproterozoic Gaofan.Hutuo and Dongjiao Groups in the Wutai and Dongjiao Areas of the North China Craton from SHRIMP U-Pb Dating of Detrital Zircons:Resolution of Debates over Their Stratigrapbic Relationships.Chinese Science Bulltin, 55(7):572-578(in Chinese). doi: 10.1007/s11434-009-0615-3?view=classic

Wang, J.P., Kusky, T., Polat, A., et al., 2013.A Late Archean Tectonic Mélange in the Central Orogenic Belt, North China Craton.Tectonophysics, 608:929-946. doi: 10.1016/j.tecto.2013.07.025

Wang, J.P., Kusky, T., Wang, L., et al., 2014.A Neoarchean Subduction Polarity Reversal Event in the North China Craton.Lithos, 220-223:133-146. http://www.sciencedirect.com/science/article/pii/S0024493715000511

Wang, K.Y., Hao, J., Wilde, S., et al., 2000.Reconsideration of Some Key Geological Problems of Late Archaean-Early Proterozoic in the Wutaishan-Hengshan Area:Constraints from SHRIMP U-Pb Zircon Data.Scientia Geologica Sinica, 35(2):175-184(in Chinese with English abstract). doi: 10.1007/s11434-009-3611-8

Wang, Y.L., Zhang, C.J., Xiu, S.Z., 2001.Th/Hf-Ta/Hf Identification of Tectonic Setting of Basalts.Acta Petrologica Sinica, 17(3):413-421(in Chinese with English abstract). https://www.researchgate.net/publication/279768841_ThHf-TaHf_idenfication_of_tectonic_setting_of_basalts

Wei, Y., Zheng, J.P., Su, Y.P, et al., 2013.Zircon U-Pb Ages and Hf Isotopes of Granulites from the Huai'an Complex:Implications for the Accretion and Reworking of the Lower Crust beneath the North Margin of the North China Craton.Acta Petrologica Sinica, 29(7):2281-2294(in Chinese with English abstract). https://www.researchgate.net/publication/285839737_Zircon_U-Pb_ages_and_Hf_isotopes_of_granulites_from_the_Huai'_an_Complex_Implications_for_the_accretion_and_reworking_of_the_lower_crust_beneath_the_north_margin_of_the_North_China_Craton

Winchester, J.A., Floyd, P.A., 1977.Geochemical Discrimination of Differenet Magma Series and Their Differentiation Products Using Immobile Elements.Chemical Geology, 20:325-343. doi: 10.1016/0009-2541(77)90057-2

Wood, D.A., 1980.The Application of a Th-Hf-Ta Diagram to Problems of Tectonomagmatic Classification and to Establishing the Nature of Crustal Contamination of Basaltic Lavas of the British Tertiary Volcanic Province.Earth and Planetary Science Letters, 50:11-30. doi: 10.1016/0012-821X(80)90116-8

Wu, C.H., Li, H.M., Zhong, C.T., et al., 2000.TIMS U-Pb Single Zircon Ages for the Orthogneiss and the Paragneiss of Fuping Complex:Implications for Existence of the Palaeoproterozoic Supracrustal Rocks in the Central Basement of North China Craton.Progress in Precambrian Research, 23(3):129-139(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZLP198901000.htm

Wu, Y.B., Chen, D.G., Xia, Q.K., et al., 2002.In-Situ Trace Element Analyses of Zircons from Dabieshan Huangzhen Eclogite:Trace Element Characteristics of Eclogite-Facies Metamorphic Zircon.Chinese Science Bulletin, 47(11):859-863(in Chinese). http://www.cqvip.com/QK/86894X/200216/1004290118.html

Wu, Y.B., Zheng, Y.F., 2004.Genesis of Zircon and Its Constraints on Interpretation of U-Pb Age.Chinese Science Bulletin, 49(16):1589-1604(in Chinese). https://www.researchgate.net/profile/Yong-Fei_Zheng/publication/225204011_Genesis_of_zircon_and_its_constraints_on_interpretation_of_U-Pb_age/links/53fe74800cf21edafd151294.pdf?origin=publication_detail

Xia, L.Q., Xia, Z.C., Xu, X.C., etal., 2007.The Discrimination between Continental Basalt and Island Arc Basalt Based on Geochemical Method.Acta Petrologica et Mineralogica, 26(1):77-88(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW200701010.htm

Xiao, L.L., Jiang, Z.S., 2010.Geochemistry and Tectonic Environment of Amphibolites of the Zanhuang Metamorphic Complex.Bulletin of Mineralogy, Petrology and Geochemistry, 29(4):339-347(in Chinese with English abstract). https://www.researchgate.net/publication/281577563_Geochemistry_and_tectonic_environment_of_amphiholites_of_the_Zanhuang_metamorphic_complex

Xiao, L.L., Liu, F.L., Liu, J.H., et al., 2013.Geochemistry and Its Tectonic Implications of the Zuoquan-Zanhuang Complex.Acta Petrologica Sinica, 29(2):533-550(in Chinese with English abstract). https://www.researchgate.net/publication/287705947_Geochemistry_and_Its_Tectonic_Implications_of_the_Zuoquan-Zanhuang_Complex

Xiao, L.L., Lu, J.S., Wang, G.D., et al., 2012.Geochemistry, Metamorphic Evolution and Its Tectonic Implications of Amphibolites in the Southwest Area of the Zanhuang Complex.Acta Petrologica Sinica, 28(9):2807-2818(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB201209012.htm

Xiao, L.L., Wang, G.D., 2011.Zircon U-Pb Dating of Metabasic Rocks in the Zanhuang Metamorphic Complex and Its Geological Significance.Acta Petrologica et Mineralogica, 30(5):781-794(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW201105005.htm

Zhai, M.G., 2011.Cratonization and the Ancient North China Continent:A Summary and Review.Science in China (Series D), 54:1110-1120. doi: 10.1007/s11430-011-4250-x

Zhang, L.C., Zhai, M.G., Zhang, X.J., et al., 2012.Formation Age and Tectonic Setting of the Shirengou Neoarchean Banded Iron Deposit in Eastern Hebei Province:Constraints from Geochemistry and SIMS Zircon U-Pb Dating.Precambrian Research, 222-223:325-338. doi: 10.1016/j.precamres.2011.09.007

Zhang, L.L., Dai, F.H., Cui, J.W., et al., 2014.Geochemistry Characteristics and Significance of Metamorphic Intrusions in Guyana Region, Inner Mongolia.Earth Science, 39(3):271-282 (in Chinese with English abstract). https://www.researchgate.net/publication/287461247_Geochemistry_characteristics_and_significance_of_metamorphic_intrusions_in_Guyang_Region_Inner_Mongolia

Zhang, Q., Qian, Q, Wang, Y., 1999.Geochemical Study on Igneous Rocks of Orogenic Belts.Earth Science Frontiers, 6(3):113-120(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GXDX200201007.htm

Zhang, R.Y., Zhang, C.L., Sun, Y., 2013.Crustal Reworking in the North China Craton at ~2.5 Ga:Evidence from Zircon U-Pb Ages, Hf Isotopes and Whole-Rock Geochemistry of the TTG Gneisses in the Zhongtiao Mountain.Acta Petrologica Sinica, 29(7):2265-2280(in Chinese with English abstract). doi: 10.1002/gj.2493/references

Zhang, Z.Q., Wu, J.S., Ye, X.J., 1991.Archaean Metamorphic Rocks from the Lower Fuping Group in the Mt.Taihang Region, North China:REE Geochemistry, Rb-Sr and Sm-Nd Ages and Implications.Geochimica, (2):118-127(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQXB198401004.htm

Zhao, G.C., 2009.Metamorphic Evolution of Major Tectonic Units in the Basement of the North China Craton:Key Issues and Discussion.Acta Petrologica Sinica, 25(8):1772-1792(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200908006.htm

Zhao, G.C., Cawood, P.A., Wilde, S.A., et al., 2002.Metamorphism of Basement Rocks in the Central Zone of the North China Craton:Implications for Paleoproterozoic Tectonic Evolution.Precambrian Research, 103:55-88. https://www.researchgate.net/profile/Guochun_Zhao/publication/222679918_Metamorphism_of_basement_rocks_in_the_Central_Zone_of_the_North_China_Craton_imphcations_for_Paleoproterozoic_tectonic_evolution/links/0912f513b5c52cf290000000.pdf?origin=publication_list

Zhao, G.C., Sun, M., Wilde, S.A., et al., 2005.Late Archean to Paleoproterozoic Evolution of the North China Craton:Key Issues Revisited.Precambrian Research, 136:177-202. doi: 10.1016/j.precamres.2004.10.002

Zhao, G.C., Wilde, S.A., Cawood, P.A., 2001.Archean Blocks and Their Boundaries in the North China Craton:Lithological, Geochemical, Structural and P-T Path Constraints and Tectonic Evolution.Precambrian Research, 107:45-73. doi: 10.1016/S0301-9268(00)00154-6

Zhao, G.C., Wilde, S.A., Cawood, P.A., et al., 1998.Thermal Evolution of the Archaean Basement Rocks from the Eastern Part of the North China Craton and Its Bearing on Tectonic Setting.International Geology Review, 40:706-721. doi: 10.1080/00206819809465233

Zhao, T.P., Zhou, M.F., Jin, C.W., et al., 2001.Discussion on Age of the Xiong'er Group in Southern Margin of North China Craton.Chinese Journal of Geology, 36(3):326-334(in Chinese with English abstract). http://hub.hku.hk/handle/10722/151066

Zhao, Z.H., 2007.How to Use the Trace Element Diagrams to Discriminate Tectonic Settings.Geotectonica et Melallogenia, 31(1):92-103(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DGYK200701012.htm

Zhao, Z.X., Du, J.F., Li, Y.H., et al., 2004.Formation of the Neoarchean Collision Orogen and Its Division of Tectonic Slices in Wutaishan Mountain.Geological Survey and Research, 27(1):5-12(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-QHWJ200401001.htm

邓晋福, 吴宗絮, 赵国春, 等, 1999.华北地台前寒武花岗岩类、陆壳演化与克拉通形成.岩石学报, 15(2): 190-198. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB902.004.htm

高劢, 高凡, 1988.张家口宣化地区太古代麻粒岩退变质作用与Rb-Sr等时年龄证据.河北地质学院学报, 11(4): 11-19. http://www.cnki.com.cn/Article/CJFDTOTAL-HBDX198804001.htm

关鸿, 孙敏, 徐平, 1998.阜平杂岩中几种不同类型片麻岩的锆石激光探针等离子体质谱年代学研究.岩石学报, 14(4): 460-470. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB804.004.htm

胡波, 翟明国, 彭澎, 等, 2013.华北克拉通古元古代末-新元古代地质事件——来自北京西山地区寒武系和侏罗系碎屑锆石LA-ICP-MS U-Pb年代学的证据.岩石学报, 29(7): 2508-2536. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201307019.htm

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://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201304028.htm

李江海, 牛向龙, 陈征, 等, 2004.太行山区深层次推覆构造的发现及其地质意义.自然科学进展, 14(10): 1118-1127. doi: 10.3321/j.issn:1002-008X.2004.10.006

刘敦一, 万渝生, 伍家善, 等, 2007.华北克拉通太古宙地壳演化和最古老的岩石.地质通报, 26(9);1131-1138. http://www.cnki.com.cn/Article/CJFDTOTAL-ZQYD200709016.htm

刘志宏, 王安建, 李晓峰, 1997.五台山晚太古代碰撞造山带的变质作用演化.高校地质学报, 3(2);162-170. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX702.003.htm

罗志波, 张华锋, 第五春荣, 等, 2012.冀西北怀安地区中性辉石麻粒岩的锆石U-Pb、Lu-Hf及微量元素组成对区域退变质时代的制约.岩石学报, 28(11): 3721-3738. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201211024.htm

孙敏, 关鸿, 2001.阜平杂岩年龄及其地质意义——兼论前寒武高级变质地体的定年问题.岩石学报, 17(1): 145-156. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200101014.htm

万渝生, 苗培森, 刘敦一, 等, 2010.华北克拉通高凡群、滹沱群和东焦群的形成时代和物质来源:碎屑锆石SHRIMP U-Pb同位素年代学制约.科学通报, 55(7): 572-578. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB201007007.htm

王凯怡, 郝杰, Simon, W., 等, 2000.山西五台山-恒山地区晚太古-早元古代若干关键地质问题的再认识:单颗粒锆石离子探针质谱年龄提出的地质制约.地质科学, 35(2): 175-184. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX200002005.htm

汪云亮, 张成江, 修淑芝, 2001.玄武岩类形成的大地构造环境的Th-Hf、Ta-Hf图解判别.岩石学报, 17(3): 413-421. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200103008.htm

魏颖, 郑建平, 苏玉平, 等, 2013.怀安麻粒岩锆石U-Pb年代学及Hf同位素:华北北缘下地壳增生再造过程研究.岩石学报, 29(7): 2281-2294. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201307003.htm

吴昌华, 李惠民, 钟长汀, 等, 2000.阜平片麻岩和湾子片麻岩的单颗粒锆石U-Pb年龄-阜平杂岩并非一统太古宙基底的年代学证据.前寒武纪研究进展, 23(3): 129-139. http://www.cnki.com.cn/Article/CJFDTOTAL-QHWJ200003000.htm

吴元保, 陈道公, 夏群科, 等, 2002.大别山黄镇榴辉岩锆石的微区微量元素分析:榴辉岩相变质锆石的微量元素特征.科学通报, 47(11): 859-863. doi: 10.3321/j.issn:0023-074X.2002.11.013

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

夏林圻, 夏祖春, 徐学义, 等, 2007.利用地球化学方法判别大陆玄武岩和岛弧玄武岩.岩石矿物学杂志, 26(1): 77-89. http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW200701010.htm

肖玲玲, 蒋宗胜, 2010.赞皇斜长角闪片岩地球化学特征及其构造环境探讨.矿物岩石地球化学通报, 29(4): 339-347. http://www.cnki.com.cn/Article/CJFDTOTAL-KYDH201004002.htm

肖玲玲, 刘福来, 刘建辉, 等, 2013.左权-赞皇变质杂岩的地球化学特征及其构造意义.岩石学报, 29(2): 533-550. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201302014.htm

肖玲玲, 卢俊生, 王国栋, 等, 2012.赞皇变质杂岩区西南部斜长角闪岩的地球化学、变质演化研究及其构造意义.岩石学报, 28(9): 2807-2818. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB201209012.htm

肖玲玲, 王国栋, 2011.赞皇变基性岩中锆石的U-Pb定年及其地质意义.岩石矿物学杂志, 30(5): 781-794. http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW201105005.htm

张莉莉, 代芳华, 崔加伟, 等, 2014.内蒙古固阳地区新太古代变质侵入岩地球化学特征及意义.地球科学, 39(3): 271-282. http://earth-science.net/WebPage/Article.aspx?id=2838

张旗, 钱青, 王焰, 1999.造山带火成岩地球化学研究.地学前缘, 6(3): 113-120. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY199903015.htm

张瑞英, 张成立, 孙勇, 2013.华北克拉通~2.5Ga地壳再造事件:来自中条山TTG质片麻岩的证据, 岩石学报, 29(7): 2265-2280. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200406003.htm

张宗清, 伍家善, 叶笑江, 1991.阜平群下部太古代变质岩石的REE、Rb-Sr和Sm-Nd年龄及其意义.地球化学, (2): 118-127. http://www.cnki.com.cn/Article/CJFDTOTAL-DQHX199102002.htm

赵国春, 2009.华北克拉通基底主要构造单元变质作用演化及其若干问题讨论.岩石学报, 25(8): 1772-1792. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200908006.htm

赵太平, 周美夫, 金成伟, 等, 2001.华北陆块南缘熊耳群形成时代讨论.地质科学, 36(3): 326-334. http://www.cnki.com.cn/Article/CJFDTOTAL-DZKX200103007.htm

赵振华, 2007.关于岩石微量元素构造环境判别图解使用的有关问题.大地构造与成矿, 31(1): 92-103. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK200701012.htm

赵祯祥, 杜晋锋, 李营辉, 等, 2004.五台山新太古代碰撞造山带的形成及构造岩片划分.地质调查与研究, 27(1): 5-12. http://www.cnki.com.cn/Article/CJFDTOTAL-QHWJ200401001.htm

Relative Articles

Relative Articles

Supplements(0)

Cited By

Cited by

Periodical cited type(11)

1.	陈贺贺，朱筱敏，施瑞生，张自力，李琪，朱珍君，阎泽昊. 断陷盆地缓坡带物源转换与沉积响应——以渤海湾盆地饶阳凹陷蠡县斜坡古近系源-汇系统为例. 石油与天然气地质. 2023(03): 689-706 .
2.	郭硕，滕学建，刘洋，滕飞，何鹏，田健，王文龙，段霄龙. 内蒙古狼山西北缘乌兰敖包地区“阿木山组”沉积时限、物源特征及其地质意义. 地球科学. 2019(01): 193-205 . 本站查看
3.	Lei Li，Wenjian Zhai. Geochemistry and Petrogenesis of the ca. 2.5Ga High-K Granitoids in the Southern North China Craton. Journal of Earth Science. 2019(03): 647-665 .
4.	田茂军，李帝铨，李斌，滕寿仁，周俊鹏. 辽宁南芬变质核杂岩核部花岗岩地球化学特征及构造意义. 地球科学. 2019(10): 3551-3564 . 本站查看
5.	陈爽，李旭平，段文勇，孙光明，冯庆达. 胶北地块斜长角闪岩的岩石学与年代学研究. 地球科学. 2018(03): 716-732 . 本站查看
6.	高山林，张仲培，刘士林，杨鑫，张福顺. 塔里木克拉通北部沙雅隆起古元古代A型花岗岩的发现及其构造意义. 岩石学报. 2018(07): 2017-2029 .
7.	陈贺贺，朱筱敏，黄捍东，施瑞生，罗亚能，崔刚. 基于碎屑锆石定年的饶阳凹陷蠡县斜坡沙河街组物源分析. 地球科学. 2017(11): 1955-1971 . 本站查看
8.	熊乐，石文杰，李欢，田宁，陈冲，周红智，赵少卿，李鹏宇. 冀东-辽西中-晚三叠世柏杖子花岗质侵入岩地球化学、Sr-Nd-Hf同位素特征及岩石成因. 地球科学. 2017(02): 207-222 . 本站查看
9.	王瑞雪，刘勇胜，宗克清，胡兆初. 内蒙古集宁橄榄岩包体微区微量元素与Sr同位素特征及其岩石圈地幔演化的指示意义. 地球科学. 2017(04): 511-526 . 本站查看
10.	蔡逸涛，倪培，王国光，陈辉，张洁. 赣东北东乡铜矿侵入岩与成矿年龄的确定及意义. 地球科学. 2017(09): 1495-1507 . 本站查看
11.	商青青，任云生，陈聪，段明新，孙琦，薛世远. 延边官地铁矿构造背景与和龙地块太古宙地壳增生:来自岩石地球化学、锆石U-Pb年代学及Hf同位素证据. 地球科学. 2017(12): 2208-2228 . 本站查看