北大别构造带始太古代片麻岩的发现

邱啸飞; 彭练红; 孔令耀; 邓新; 王达; 陈伟雄; 吴年文; 童喜润; 田洋; 牛志军

doi:10.3799/dqkx.2023.040

北大别构造带始太古代片麻岩的发现

doi: 10.3799/dqkx.2023.040

邱啸飞^1, ,,
彭练红¹,
孔令耀²,
邓新¹,
王达^{3, 4},
陈伟雄^{1, 5},
吴年文¹,
童喜润¹,
田洋¹,
牛志军¹

1.
中国地质调查局武汉地质调查中心, 湖北武汉 430205
2.
湖北省地质调查研究院, 湖北武汉 430074
3.
美国卡内基科学研究所, 华盛顿 20015
4.
成都理工大学, 四川成都 610059
5.
中国地质大学, 湖北武汉 430074

基金项目:

国家自然科学基金项目 42272229

国家自然科学基金项目 U2344210

武汉地质调查中心“潜龙计划”青年拔尖人才项目 QL2022-02

详细信息

作者简介:
邱啸飞（1985-），男，研究员，博士，主要从事华南陆块前寒武纪地质学研究.ORCID：0000-0001-8770-813X.E-mail：qiuxiaofei@mail.cgs.gov.cn

中图分类号: P58
计量
- 文章访问数: 363
- HTML全文浏览量: 204
- PDF下载量: 91
- 被引次数: 0
出版历程
- 收稿日期: 2023-02-07
- 刊出日期: 2024-11-25

Discovery of Eoarchean Gneisses in Northern Dabie Belt

1.
Wuhan Center of China Geological Survey, Wuhan 430205, China
2.
Hubei Geological Survey, Wuhan 430074, China
3.
Carnegie Institution for Science, Washington D.C. 20015, USA
4.
Chengdu University of Technology, Chengdu 610059, China
5.
China University of Geosciences, Wuhan 430074, China

摘要

摘要: 始太古代岩石因其稀缺性，对于理解最早期陆壳形成和演化具有重要意义.报道了大别造山带北大别构造带内新识别出的一套英云闪长片麻岩和斜长角闪片麻岩组合的锆石年龄，并将其命名为“木子店片麻杂岩”.定年结果显示，斜长角闪片岩和英云闪长片麻岩的锆石年龄分别为（3 653±43）Ma和（3 701±29）Ma，为目前扬子克拉通已发现的最古老岩石，说明扬子克拉通之下可能存在极为古老的基底岩石.与崆岭杂岩基底岩石的对比研究显示，木子店片麻杂岩在岩石类型以及时代上与崆岭杂岩均存在明显差异，说明崆岭杂岩和木子店片麻杂岩可能代表了扬子克拉通内相互独立的微陆块古陆核.
- 始太古代 /
- 木子店片麻杂岩 /
- 扬子克拉通 /
- 北大别构造带 /
- 英云闪长片麻岩 /
- 构造地质学 /
- 岩石学
Abstract: Eoarchean rocks are of great significance for understanding the formation and evolution of the earliest continental crust due to their scarcity. In this study, it reports zircon U-Pb ages of a newly recognized tonalitic gneiss and plagioclase-amphibolitic gneiss assemblage in the northern Dabie belt, which is named as the "Muzidian gneiss complex". The zircon dating results show that the ages of the plagioclase-amphibolitic schist and tonalitic gneiss in the Muzidian gneiss complex are (3 653±43) Ma and (3 701±29) Ma, respectively, which are the oldest rocks known in the Yangtze craton, indicating ancient basement rocks may exist beneath the craton. A comparative study with the basement rocks of the Kongling complex reveals that both the lithology and age of the Muzidian gneiss complex are distinct from those of the Kongling complex, indicating that they may represent independent microcontinental nucleus of the Yangtze craton.
- Eoarchean /
- Muzidian gneiss complex /
- Yangtze craton /
- northern Dabie belt /
- tonalitic gneiss /
- tectonics /
- petrology

HTML全文

图 1 木子店地区区域地质简图(据Qiu et al., 2021b修改)

Fig. 1. geological map for the Muzidian area and sampling location (modified after Qiu et al., 2021b)

下载: 全尺寸图片幻灯片

图 2 木子店片麻杂岩斜长角闪片岩(a, c)和英云闪长片麻岩(b, d)野外和镜下照片

Pl.斜长石；Hb.角闪石；Cpx.单斜辉石；Bi.黑云母；Q.石英

Fig. 2. Field outcrop and photomicrograph for the plagioclase-amphibolitic schist (a, c) and tonalitic gneiss (b, d) from the Muzidian gneiss complex

下载: 全尺寸图片幻灯片

图 3 北大别木子店片麻杂岩代表性锆石阴极发光图

a.斜长角闪片岩（21MZD21）；b.英云闪长片麻岩（22DW21）

Fig. 3. CL images of representative zircons for the Muzidian gneiss complex in the northern Dabie belt

下载: 全尺寸图片幻灯片

图 4 北大别木子店片麻杂岩锆石U-Pb年龄谐和图

a.斜长角闪片岩（21MZD21）；b.英云闪长片麻岩（22DW21）

Fig. 4. U-Pb concordia diagrams of zircons from the Muzidian gneiss complex in the northern Dabie belt

下载: 全尺寸图片幻灯片

参考文献(67)

Bauer, A. M., Fisher, C. M., Vervoort, J. D., et al., 2017. Coupled Zircon Lu-Hf and U-Pb Isotopic Analyses of the Oldest Terrestrial Crust, the > 4.03 Ga Acasta Gneiss Complex. Earth and Planetary Science Letters, 458: 37-48. https://doi.org/10.1016/j.epsl.2016.10.036
Boehnke, P., Bell, E. A., Stephan, T., et al., 2018. Potassic, High-Silica Hadean Crust. Proceedings of the National Academy of Sciences of the United States of America, 115(25): 6353-6356. https://doi.org/10.1073/pnas.1720880115
Bowring, S. A., Williams, I. S., 1999. Priscoan (4.00-4.03 Ga) Orthogneisses from Northwestern Canada. Contributions to Mineralogy and Petrology, 134(1): 3-16. https://doi.org/10.1007/s004100050465
Chen, Q., Sun, M., Zhao, G. C., et al., 2019. Episodic Crustal Growth and Reworking of the Yudongzi Terrane, South China: Constraints from the Archean TTGS and Potassic Granites and Paleoproterozoic Amphibolites. Lithos, 326: 1-18. https://doi.org/10.1016/j.lithos.2018.12.005
Cui, X. Z., Ren, G. M., Sun, Z. M., et al., 2020. Multiple Tectonothermal Events Recorded in the Early Precambrian Cuoke Complex in the Southwestern Yangtze Block, South China. Earth Science, 45(8): 3054-3069 (in Chinese with English abstract).
David, J., Godin, L., Stevenson, R., et al., 2009. U-Pb Ages (3.8-2.7 Ga) and Nd Isotope Data from the Newly Identified Eoarchean Nuvvuagittuq Supracrustal Belt, Superior Craton, Canada. Geological Society of America Bulletin, 121: 150-163.
Diwu, C. R., Sun, Y., Guo, A. L., 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(1): 149-170. https://doi.org/10.1016/j.gr.2011.01.011
Gao, S., Yang, J., Zhou, L., et al., 2011. Age and Growth of the Archean Kongling Terrain, South China, with Emphasis on 3.3 Ga Granitoid Gneisses. American Journal of Science, 311(2): 153-182. https://doi.org/10.2475/02.2011.03
Ge, R. F., Wilde, S. A., Kemp, A. I. S., et al., 2020. Generation of Eoarchean Continental Crust from Altered Mafic Rocks Derived from a Chondritic Mantle: The ∼3.72 Ga Aktash Gneisses, Tarim Craton (NW China). Earth and Planetary Science Letters, 538: 116225. https://doi.org/10.1016/j.epsl.2020.116225
Ge, R. F., Zhu, W. B., Wilde, S. A., et al., 2018. Remnants of Eoarchean Continental Crust Derived from a Subducted Proto-Arc. Science Advances, 4(2): eaao3159. https://doi.org/10.1126/sciadv.aao3159
Guo, J. L., Gao, S., Wu, Y. B., et al., 2014.3. 45 Ga Granitic Gneisses from the Yangtze Craton, South China: Implications for Early Archean Crustal Growth. Precambrian Research, 242: 82-95. https://doi.org/10.1016/j.precamres.2013.12.018
Hacker, B. R., Ratschbacher, L., Webb, L., et al., 1998. U/Pb Zircon Ages Constrain the Architecture of the Ultrahigh-Pressure Qinling-Dabie Orogen, China. Earth and Planetary Science Letters, 161(1/2/3/4): 215-230. https://doi.org/10.1016/S0012-821X(98)00152-6
Han, Q. S., Peng, S. B., Kusky, T., et al., 2017. A Paleoproterozoic Ophiolitic Mélange, Yangtze Craton, South China: Evidence for Paleoproterozoic Suturing and Microcontinent Amalgamation. Precambrian Research, 293: 13-38. https://doi.org/10.1016/j.precamres.2017.03.004
Harrison, T. M., Bell, E. A., Boehnke, P., 2017. Hadean Zircon Petrochronology. Reviews in Mineralogy and Geochemistry, 83(1): 329-363. https://doi.org/10.2138/rmg.2017.83.11
Hawkesworth, C., Cawood, P. A., Dhuime, B., 2019. Rates of Generation and Growth of the Continental Crust. Geoscience Frontiers, 10(1): 165-173. https://doi.org/10.1016/j.gsf.2018.02.004
Hu, J. L., Liu, J. S., Liu, A. S., et al., 2018. Age and Petrogenesis of the Porphyritic Biotite Monzogranite in the Muzidian Complex in Northern Dabie Mountains: Evidences from Zircon U-Pb Dating, Hf Isotopes and REE Geochemistry. Bulletin of Mineralogy, Petrology and Geochemistry, 37(4): 750-759 (in Chinese with English abstract).
Hu, J., Liu, X. C., Chen, L. Y., et al., 2013. A ∼2.5 Ga Magmatic Event at the Northern Margin of the Yangtze Craton: Evidence from U-Pb Dating and Hf Isotope Analysis of Zircons from the Douling Complex in the South Qinling Orogen. Chinese Science Bulletin, 58(28): 3564-3579. https://doi.org/10.1007/s11434-013-5904-1
Hui, B., Dong, Y. P., Cheng, C., et al., 2017. Zircon U-Pb Chronology, Hf Isotope Analysis and Whole-Rock Geochemistry for the Neoarchean-Paleoproterozoic Yudongzi Complex, Northwestern Margin of the Yangtze Craton, China. Precambrian Research, 301: 65-85. https://doi.org/10.1016/j.precamres.2017.09.003
Jiang, L. L., Wu, W. P., Hu, L. J., et al., 2000. Tectonic Setting of the North Dabie Complex in the Dabie Mountains. Geoscience, 14(1): 29-36 (in Chinese with English abstract).
Jiao, W. F., Wu, Y. B., Yang, S. H., et al., 2009. The Oldest Basement Rock in the Yangtze Craton Revealed by Zircon U-Pb Age and Hf Isotope Composition. Science in China (Series D: Earth Sciences), 52(9): 1393-1399. https://doi.org/10.1007/s11430-009-0135-7
Li, Z. S., Shan, X. L., Liu, J., et al., 2023. Late Neoarchean TTG and Monzogranite in the Northeastern North China Craton: Implications for Partial Melting of a Thickened Lower Crust. Gondwana Research, 115: 201-223. https://doi.org/10.1016/j.gr.2022.10.008
Liu, D. Y., Nutman, A. P., Compston, W., et al., 1992. Remnants of ≥3 800 Ma Crust in the Chinese Part of the Sino-Korean Craton. Geology, 20(4): 339. https://doi.org/10.1130/0091-7613(1992)0200339: romcit>2.3.co;2 doi: 10.1130/0091-7613(1992)0200339:romcit>2.3.co;2
Liu, Y. S., Zong, K. Q., Kelemen, P. B., et al., 2008. Geochemistry and Magmatic History of Eclogites and Ultramafic Rocks from the Chinese Continental Scientific Drill Hole: Subduction and Ultrahigh-Pressure Metamorphism of Lower Crustal Cumulates. Chemical Geology, 247(1-2): 133-153. https://doi.org/10.1016/j.chemgeo.2007.10.016
Ludwig, K. R., 2003. ISOPLOT 3.0: A Geochronological Toolkit for Microsoft Excel. BGC Special Publication 1a, Berkeley, 55.
Ma, Q., Xu, Y. G., Huang, X. L., et al., 2020. Eoarchean to Paleoproterozoic Crustal Evolution in the North China Craton: Evidence from U-Pb and Hf-O Isotopes of Zircons from Deep-Crustal Xenoliths. Geochimica et Cosmochimica Acta, 278: 94-109. https://doi.org/10.1016/j.gca.2019.09.009
Nie, H., Yao, J., Wan, X., et al., 2016. Precambrian Tectonothermal Evolution of South Qinling and Its Affinity to the Yangtze Block: Evidence from Zircon Ages and Hf-Nd Isotopic Compositions of Basement Rocks. Precambrian Research, 286: 167-179. https://doi.org/10.1016/j.precamres.2016.10.005
Nutman, A. P., Friend, C. R. L., Paxton, S., 2009. Detrital Zircon Sedimentary Provenance Ages for the Eoarchaean Isua Supracrustal Belt Southern West Greenland: Juxtaposition of an Imbricated ca. 3 700 Ma Juvenile Arc against an Older Complex with 3 920-3 760 Ma Components. Precambrian Research, 172(3/4): 212-233. https://doi.org/10.1016/j.precamres.2009.03.019
Qiu, X. F., 2022. Pre-Devonian Crustal Evolution of the Northern Yangtze Craton: Evidence from U-Pb Ages and Hf Isotopes of Detrital Zircons. Acta Geologica Sinica, 96(11): 3784-3798 (in Chinese with English abstract).
Qiu, X. F., Chen, W. X., Xu, D. L., et al., 2022. Crustal Evolution in Archean for the Kongling Complex in the Yangtze Craton Nucleus. South China Geology, 38(1): 56-66 (in Chinese with English abstract).
Qiu, X. F., Deng, X., Jiang, T., et al., 2021a. First Discovery of Hadean Xenocrystal Zircons from Granitic Gneisses in the Northern Dabie Orogen. Acta Geologica Sinica, 95(5): 1775-1776. https://doi.org/10.1111/1755-6724.14755
Qiu, X. F., Tong, X. R., Jiang, T., et al., 2021b. Reworking of Hadean Continental Crust in the Dabie Orogen: Evidence from the Muzidian Granitic Gneisses. Gondwana Research, 89: 119-130. https://doi.org/10.1016/j.gr.2020.08.014
Qiu, X. F., Jiang, T., Wu, N. W., et al., 2020. Neoarchean Crustal Rocks and Paleoproterozoic Migmatization in the Dabie Orogen: Evidence from Zircon U-Pb Age and Hf Isotopes. Acta Geologica Sinica, 94(3): 729-738 (in Chinese with English abstract).
Qiu, X. F., Ling, W. L., Liu, X. M., et al., 2011. Recognition of Grenvillian Volcanic Suite in the Shennongjia Region and Its Tectonic Significance for the South China Craton. Precambrian Research, 191(3/4): 101-119. https://doi.org/10.1016/j.precamres.2011.09.011
Ren, G. M., Pang, W. H., Wang, L. Q., et al., 2020. Detrital Zircons of 3.8 Ga in Southwestern Yangtze Block and Its Geological Implications. Earth Science, 45(8): 3040-3053 (in Chinese with English abstract).
Sun, M., Chen, N., Zhao, G., et al., 2008. U-Pb Zircon and Sm-Nd Isotopic Study of the Huangtuling Granulite, Dabie-Sulu Belt, China: Implication for the Paleoproterozoic Tectonic History of the Yangtze Craton. American Journal of Science, 308(4): 469-483. https://doi.org/10.2475/04.2008.03
Tian, Y., Wang, W., Jin, W., et al., 2022. Neoarchean Granitic Rocks from the Jiamiao Area of the Dabie Orogen: Implications on the Formation and Early Evolution of the Yangtze Craton. Science China Earth Sciences, 65(8): 1568-1585. https://doi.org/10.1007/s11430-021-9935-5
Tu, C., Zhang, S. B., Su, K., et al., 2021. Zircon U-Pb Dating and Lu-Hf Isotope Results for Feidong Complex: Implications for Coherent Basement of the Yangtze Craton. Earth Science, 46(5): 1630-1643 (in Chinese with English abstract).
Wan, Y. S., 2022. How to Form the Oldest Continental Crust?. Earth Science, 47(10): 3776-3778 (in Chinese).
Wan, Y. S., Liu, D. Y., Dong, C. Y., et al., 2009. The Oldest Rocks and Zircons in China. Acta Petrologica Sinica, 25(8): 1793-1807 (in Chinese with English abstract).
Wan, Y. S., Xie, H. Q., Dong, C. Y., et al., 2019. Hadean to Paleoarchean Rocks and Zircons in China. In: Kranendonk, M. J. V., ed., Earth's Oldest Rocks (Second Edition). Elsevier, Amsterdam, 293-327.
Wan, Y. S., Xie, H. Q., Wang, H. C., et al., 2021. Discovery of ~3.8 Ga TTG Rocks in Eastern Hebei, North China Craton. Acta Geologica Sinica, 95(5): 1321-1333 (in Chinese with English abstract).
Wang, K., Dong, S. W., Li, Z. X., et al., 2018. Age and Chemical Composition of Archean Metapelites in the Zhongxiang Complex and Implications for Early Crustal Evolution of the Yangtze Craton. Lithos, 320: 280-301. https://doi.org/10.1016/j.lithos.2018.09.027
Wang, Z. J., Wang, J., Du, Q. D., et al., 2013. The Evolution of the Central Yangtze Block during Early Neoarchean Time: Evidence from Geochronology and Geochemistry. Journal of Asian Earth Sciences, 77: 31-44. https://doi.org/10.1016/j.jseaes.2013.08.013
Wu, Y. B., Zheng, Y. F., Gao, S., et al., 2008. Zircon U-Pb Age and Trace Element Evidence for Paleoproterozoic Granulite-Facies Metamorphism and Archean Crustal Rocks in the Dabie Orogen. Lithos, 101(3/4): 308-322. https://doi.org/10.1016/j.lithos.2007.07.008
Wu, Y. B., Zheng, Y. F., Zhang, S. B., et al., 2007. Zircon U-Pb Ages and Hf Isotope Compositions of Migmatite from the North Dabie Terrane in China: Constraints on Partial Melting. Journal of Metamorphic Geology, 25(9): 991-1009. https://doi.org/10.1111/j.1525-1314.2007.00738.x
Wu, Y. B., Zhou, G. Y., Gao, S., et al., 2014. Petrogenesis of Neoarchean TTG Rocks in the Yangtze Craton and Its Implication for the Formation of Archean TTGS. Precambrian Research, 254: 73-86. https://doi.org/10.1016/j.precamres.2014.08.004
Yang, C., Wei, C. J., 2017. Two Phases of Granulite Facies Metamorphism during the Neoarchean and Paleoproterozoic in the East Hebei, North China Craton: Records from Mafic Granulites. Precambrian Research, 301: 49-64. https://doi.org/10.1016/j.precamres.2017.09.005
Zhai, M. G., Zhao, L., Zhu, X. Y., et al., 2020. Review and Overview for the Frontier Hotspot: Early Continents and Start of Plate Tectonics. Acta Petrologica Sinica, 36(8): 2249-2275 (in Chinese with English abstract).
Zhang, S. B., Zheng, Y. F., Wu, P., et al., 2020. The Nature of Subduction System in the Neoarchean: Magmatic Records from the Northern Yangtze Craton, South China. Precambrian Research, 347: 105834.
Zhang, S. B., Zheng, Y. F., Wu, Y. B., et al., 2006. Zircon U-Pb Age and Hf Isotope Evidence for 3.8 Ga Crustal Remnant and Episodic Reworking of Archean Crust in South China. Earth and Planetary Science Letters, 252(1-2): 56-71. https://doi.org/10.1016/j.epsl.2006.09.027
Zhao, T. Y., Li, J., Liu, G. C., et al., 2020. Petrogenesis of Archean TTGS and Potassic Granites in the Southern Yangtze Block: Constraints on the Early Formation of the Yangtze Block. Precambrian Research, 347: 105848. https://doi.org/10.1016/j.precamres.2020.105848
Zheng, J. P., Griffin, W. L., O'Reilly, S. Y., et al., 2004. 3.6 Ga Lower Crust in Central China: New Evidence on the Assembly of the NCC. Geology, 32: 229-332.
Zheng, Y. F., Zhao, G. C., 2020. Two Styles of Plate Tectonics in Earth's History. Science Bulletin, 65(4): 329-334. https://doi.org/10.1016/j.scib.2018.12.029
Zhou, G. Y., Wu, Y. B., Gao, S., et al., 2015. The 2.65 Ga A-Type Granite in the Northeastern Yangtze Craton: Petrogenesis and Geological Implications. Precambrian Research, 258: 247-259. https://doi.org/10.1016/j.precamres.2015.01.003
Zhou, K., Chen, Y. X., Zhang, S. B., et al., 2020. Zircon Evidence for the Eoarchean (~3.7 Ga) Crustal Remnant in the Sulu Orogen, Eastern China. Precambrian Research, 337: 105529. https://doi.org/10.1016/j.precamres.2019.105529
崔晓庄, 任光明, 孙志明, 等, 2020. 扬子陆块西南缘早前寒武纪撮科杂岩记录的多期岩浆‒变质事件. 地球科学, 45(8): 3054-3069.
胡俊良, 刘劲松, 刘阿睢, 等, 2018. 北大别木子店岩体斑状黑云二长花岗岩的年龄与成因: 锆石U-Pb定年、Hf同位素与稀土元素证据. 矿物岩石地球化学通报, 37(4): 750-759.
江来利, 吴维平, 胡礼军, 等, 2000. 大别山北大别杂岩的大地构造属性. 现代地质, 14(1): 29-36.
邱啸飞, 2022. 扬子克拉通北部前泥盆纪地壳演化: 来自碎屑锆石U-Pb和Hf同位素证据. 地质学报, 96(11): 3784-3798.
邱啸飞, 陈伟雄, 徐大良, 等, 2022. 扬子陆核崆岭杂岩太古宙地壳演化. 华南地质, 38(1): 56-66.
邱啸飞, 江拓, 吴年文, 等, 2020. 大别造山带新太古代地壳岩石和古元古代混合岩化作用——来自锆石U-Pb年代学和Hf同位素证据. 地质学报, 94(3): 729-738.
任光明, 庞维华, 王立全, 等, 2020. 扬子陆块西南缘3.8 Ga碎屑锆石及其地质意义. 地球科学, 45(8): 3040-3053.
涂城, 张少兵, 苏克, 等, 2021. 肥东杂岩锆石U-Pb年龄和Lu-Hf同位素: 对扬子克拉通统一结晶基底的限制. 地球科学, 46(5): 1630-1643.
万渝生, 2022. 最古老陆壳是如何形成的?. 地球科学, 47(10): 3776-3778.
万渝生, 刘敦一, 董春艳, 等, 2009. 中国最老岩石和锆石. 岩石学报, 25(8): 1793-1807.
万渝生, 颉颃强, 王惠初, 等, 2021. 冀东地区~3.8 Ga TTG岩石发现. 地质学报, 95(5): 1321-1333.
翟明国, 赵磊, 祝禧艳, 等, 2020. 早期大陆与板块构造启动: 前沿热点介绍与展望. 岩石学报, 36(8): 2249-2275.