• 中国出版政府奖提名奖

    中国百强科技报刊

    湖北出版政府奖

    中国高校百佳科技期刊

    中国最美期刊

    留言板

    尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

    姓名
    邮箱
    手机号码
    标题
    留言内容
    验证码

    大陆板片-地幔相互作用:来自大别造山带碰撞后安山质火山岩的地球化学证据

    赵子福 代富强 陈启

    赵子福, 代富强, 陈启, 2019. 大陆板片-地幔相互作用:来自大别造山带碰撞后安山质火山岩的地球化学证据. 地球科学, 44(12): 4119-4127. doi: 10.3799/dqkx.2019.244
    引用本文: 赵子福, 代富强, 陈启, 2019. 大陆板片-地幔相互作用:来自大别造山带碰撞后安山质火山岩的地球化学证据. 地球科学, 44(12): 4119-4127. doi: 10.3799/dqkx.2019.244
    Zhao Zifu, Dai Fuqiang, Chen Qi, 2019. Continental Slab-Mantle Interaction: Geochemical Evidence from Post-Collisional Andesitic Rocks in the Dabie Orogen. Earth Science, 44(12): 4119-4127. doi: 10.3799/dqkx.2019.244
    Citation: Zhao Zifu, Dai Fuqiang, Chen Qi, 2019. Continental Slab-Mantle Interaction: Geochemical Evidence from Post-Collisional Andesitic Rocks in the Dabie Orogen. Earth Science, 44(12): 4119-4127. doi: 10.3799/dqkx.2019.244

    大陆板片-地幔相互作用:来自大别造山带碰撞后安山质火山岩的地球化学证据

    doi: 10.3799/dqkx.2019.244
    基金项目: 

    国家“973”计划项目 2015CB856102

    详细信息
      作者简介:

      赵子福(1973-), 男, 教授, 博士生导师, 地球化学专业

    • 中图分类号: P597

    Continental Slab-Mantle Interaction: Geochemical Evidence from Post-Collisional Andesitic Rocks in the Dabie Orogen

    • 摘要: 俯冲到地幔深度的地壳物质不可避免地在板片-地幔界面与地幔楔发生相互作用,由此形成的超镁铁质交代岩就是造山带镁铁质火成岩的地幔源区.因此,造山带镁铁质火成岩为研究俯冲地壳物质再循环和壳-幔相互作用提供了重要研究对象.为了揭示俯冲陆壳物质再循环的机制和过程,对大别造山带碰撞后安山质火山岩开展了元素和同位素地球化学研究.这些安山质火山岩的SIMS锆石U-Pb年龄为124±3~130±2 Ma,表明其形成于早白垩世.此外,残留锆石的U-Pb年龄为中新元古代和三叠纪,分别对应于大别-苏鲁造山带超高压变火成岩的原岩年龄和变质年龄.它们具有岛弧型微量元素特征、富集的Sr-Nd-Hf同位素组成,以及变化的且大多不同于正常地幔的锆石δ18O值.这些元素和同位素特征指示,这些安山质火山岩是交代富集的造山带岩石圈地幔部分熔融的产物.在三叠纪华南陆块俯冲于华北陆块之下的过程中,俯冲华南陆壳来源的长英质熔体交代了上覆华北岩石圈地幔楔橄榄岩,大陆俯冲隧道内的熔体-橄榄岩反应产生了富沃、富集的镁铁质地幔交代岩.这种地幔交代岩在早白垩世发生部分熔融,就形成了所观察到的安山质火山岩.因此,碰撞造山带镁铁质岩浆岩的地幔源区是通过大陆俯冲隧道内板片-地幔相互作用形成的,而加入地幔楔中长英质熔体的比例决定了这些镁铁质岩浆岩的岩石化学和地球化学成分.

       

    • 图  1  大别造山带碰撞后安山质火山岩锆石δ18O值(a)和残留锆石U-Pb年龄(b)统计图

      Dai et al.(2016);正常地幔锆石δ18O为5.3‰±0.3‰(Valley et al., 1998)

      Fig.  1.  Histograms of zircon δ18O values (a) and relict zircon U-Pb ages (b) for post-collisional andesitic rocks in the Dabie orogen

      图  2  大别造山带碰撞后安山质火山岩全岩Na2O+K2O-SiO2(TAS)图(a)、Sr-Nd同位素组成图(b)、稀土(c)和微量元素(d)分布图

      Dai et al., (2016);LM.华北岩石圈地幔;CDB.中大别超高压变质岩;NDB.北大别超高压变质岩;PCMI.大别造山带碰撞后镁铁质-超镁铁质侵入岩;PCG.大别造山带碰撞后花岗岩

      Fig.  2.  Plots of whole-rock Na2O+K2O-SiO2 (TAS) (a), Sr-Nd isotope compositions (b), REE (c) and trace element (d) distribution patterns for post-collisional andesitic rocks in the Dabie orogen

      图  3  大陆俯冲隧道板片-地幔相互作用和大别造山带碰撞后安山质火山作用示意

      a.三叠纪,俯冲华南陆壳衍生的长英质熔体与上覆华北岩石圈地幔楔橄榄岩反应,产生镁铁质-超镁铁质地幔交代岩;b.早白垩世,这些交代岩发生部分熔融,形成碰撞后安山质火山岩和镁铁质-超镁铁质侵入岩;UM.超镁铁质交代岩,MM.镁铁质交代岩.据Dai et al.(2016)

      Fig.  3.  Schematic cartoons illustrating the slab-mantle interaction in continental subduction channel and the post-collisional andesitic volcanism in the Dabie orogen, East-Central China

    • Chen, L., Zhao, Z.F., 2017.Origin of Continental Arc Andesites:The Composition of Source Rocks is the Key.Journal of Asian Earth Sciences, 145:217-232. https://doi.org/10.1016/j.jseaes.2017.04.012
      Chen, L., Zhao, Z.F., Zheng, Y.F., 2014.Origin of Andesitic Rocks:Geochemical Constraints from Mesozoic Volcanics in the Luzong Basin, South China.Lithos, 190-191:220-239. https://doi.org/10.1016/j.lithos.2013.12.011
      Chopin, C., 1984.Coesite and Pure Pyrope in High-Grade Blueschists of the Western Alps:A First Record and Some Consequences.Contributions to Mineralogy and Petrology, 86(2):107-118. doi: 10.1007/BF00381838
      Cloos, M., Shreve, R.L., 1988a.Subduction-Channel Model of Prism Accretion, Melange Formation, Sediment Subduction, and Subduction Erosion at Convergent Plate Margins:1.Background and Description.Pure and Applied Geophysics PAGEOPH, 128(3-4):455-500. doi: 10.1007/BF00874548
      Cloos, M., Shreve, R.L., 1988b.Subduction-Channel Model of Prism Accretion, Melange Formation, Sediment Subduction, and Subduction Erosion at Convergent Plate Margins:2.Implications and Discussion.Pure and Applied Geophysics PAGEOPH, 128(3-4):501-545. doi: 10.1007/BF00874549
      Dai, F.Q., Zhao, Z.F., Dai, L.Q., et al., 2016.Slab-Mantle Interaction in the Petrogenesis of Andesitic Magmas:Geochemical Evidence from Postcollisional Intermediate Volcanic Rocks in the Dabie Orogen, China.Journal of Petrology, 57(6):1109-1134. https://doi.org/10.1093/petrology/egw034
      Dai, F.Q., Zhao, Z.F., Zheng, Y.F., 2017a.Partial Melting of the Orogenic Lower Crust:Geochemical Insights from Post-Collisional Alkaline Volcanics in the Dabie Orogen.Chemical Geology, 454:25-43. https://doi.org/10.1016/j.chemgeo.2017.02.022
      Dai, F.Q., Zhao, Z.F., Zheng, Y.F., et al., 2019.The Geochemical Nature of Mantle Sources for Two Types of Cretaceous Basaltic Rocks from Luxi and Jiaodong in East-Central China.Lithos, 344-345:409-424. https://doi.org/10.1016/j.lithos.2019.07.007
      Dai, L.Q., Zhao, Z.F., Zheng, Y.F., 2014.Geochemical Insights into the Role of Metasomatic Hornblendite in Generating Alkali Basalts.Geochemistry, Geophysics, Geosystems, 15(10):3762-3779. https://doi.org/10.1002/2014gc005486
      Dai, L.Q., Zhao, Z.F., Zheng, Y.F., 2015.Tectonic Development from Oceanic Subduction to Continental Collision:Geochemical Evidence from Postcollisional Mafic Rocks in the Hong'an-Dabie Orogens.Gondwana Research, 27(3):1236-1254. doi: 10.1016/j.gr.2013.12.005
      Dai, L.Q., Zhao, Z.F., Zheng, Y.F., et al., 2011.Zircon Hf-O Isotope Evidence for Crust-Mantle Interaction during Continental Deep Subduction.Earth and Planetary Science Letters, 308(1):229-244. https://doi.org/10.1016/j.epsl.2011.06.001.
      Dai, L.Q., Zhao, Z.F., Zheng, Y.F., et al., 2012.The Nature of Orogenic Lithospheric Mantle:Geochemical Constraints from Postcollisional Mafic-Ultramafic Rocks in the Dabie Orogen.Chemical Geology, 334:99-121. https://doi.org/10.1016/j.chemgeo.2012.10.009
      Dai, L.Q., Zhao, Z.F., Zheng, Y.F., et al., 2017b.Geochemical Distinction between Carbonate and Silicate Metasomatism in Generating the Mantle Sources of Alkali Basalts.Journal of Petrology, 58(5):863-884. https://doi.org/10.1093/petrology/egx038
      Dai, L.Q., Zheng, F., Zhao, Z.F., et al., 2017c.Recycling of Paleotethyan Oceanic Crust:Geochemical Record from Postcollisional Mafic Igneous Rocks in the Tongbai-Hong'an Orogens.Geological Society of America Bulletin, 129(1-2):179-192. https://doi.org/10.1130/b31461.1
      Fan, W.M., Guo, F., Wang, Y.J., et al., 2004.Late Mesozoic Volcanism in the Northern Huaiyang Tectono-Magmatic Belt, Central China:Partial Melts from a Lithospheric Mantle with Subducted Continental Crust Relicts beneath the Dabie Orogen? Chemical Geology, 209(1-2):27-48. https://doi.org/10.1016/j.chemgeo.2004.04.020
      Gómez-Tuena, A., Straub, S.M., Zellmer, G.F., 2014.An Introduction to Orogenic Andesites and Crustal Growth.Geological Society, London, Special Publications, 385(1):1-13. https://doi.org/10.1144/sp385.16
      Hacker, B.R., Kelemen, P.B., Behn, M.D., 2011.Differentiation of the Continental Crust by Relamination.Earth and Planetary Science Letters, 307(3-4):501-516. https://doi.org/10.1016/j.epsl.2011.05.024
      Hawkesworth, C.J., Hergt, J.M., Ellam, R.M., et al., 1991.Element Fluxes Associated with Subduction Related Magmatism.Philosophical Transactions of the Royal Society, 335(1638):393-405. https://doi.org/10.1098/rsta.1991.0054
      Hildreth, W., Moorbath, S., 1988.Crustal Contributions to Arc Magmatism in the Andes of Central Chile.Contributions to Mineralogy and Petrology, 98(4):455-489. https://doi.org/10.1007/BF00372365
      Hirose, K., 1997.Melting Experiments on Lherzolite KLB-1 under Hydrous Conditions and Generation of High Magnesian Andesitic Melts.Geology, 25(1):42-44. doi: 10.1130/0091-7613(1997)025<0042:MEOLKU>2.3.CO;2
      Hofmann, A.W., 1988.Chemical Differentiation of the Earth:The Relationship between Mantle, Continental Crust, and Oceanic Crust.Earth and Planetary Science Letters, 90(3):297-314. doi: 10.1016/0012-821X(88)90132-X
      Hofmann, A.W., 1997.Mantle Geochemistry:The Message from Oceanic Volcanism.Nature, 385:219-229. https://doi.org/10.1038/385219a0
      Kelemen, P.B., Hanghøj, K., Greene, A.R., 2007.One View of the Geochemistry of Subduction-Related Magmatic Arcs, with an Emphasis on Primitive Andesite and Lower Crust.Treatise on Geochemistry, 3:1-70. https://doi.org/10.1016/b0-08-043751-6/03035-8
      Lee, C.T.A., 2014.Physics and Chemistry of Deep Continental Crust Recycling.Treatise on Geochemistry, 4:423-456. https://doi.org/10.1016/b978-0-08-095975-7.00314-4
      Lee, C.T.A., Morton, D.M., Kistler, R.W., et al., 2007.Petrology and Tectonics of Phanerozoic Continent Formation:From Island Arcs to Accretion and Continental Arc Magmatism.Earth and Planetary Science Letters, 263(3-4):370-387. https://doi.org/10.1016/j.epsl.2007.09.025
      Niu, Y.L., Zhao, Z.D., Zhu, D.C., et al., 2013.Continental Collision Zones are Primary Sites for Net Continental Crust Growth:A Testable Hypothesis.Earth-Science Reviews, 127:96-110. https://doi.org/10.1016/j.earscirev.2013.09.004
      Peacock, S.M., 1993.The Importance of Blueschist-Eclogite Dehydration Reactions in Subducting Oceanic Crust.Geological Society of America Bulletin, 105(5):684-694. doi: 10.1130/0016-7606(1993)105<0684:TIOBED>2.3.CO;2
      Reubi, O., Blundy, J., 2009.A Dearth of Intermediate Melts at Subduction Zone Volcanoes and the Petrogenesis of Arc Andesites.Nature, 461:1269-1273. https://doi.org/10.1038/nature08510
      Rudnick, R.L., Gao, S., 2014.Composition of the Continental Crust.Treatise on Geochemistry.4:1-51. https://doi.org/10.1016/b978-0-08-095975-7.00301-6
      Rumble, D., Liou, J.G., Jahn, B.M., 2003.Continental Crust Subduction and Ultrahigh Pressure Metamorphism.Treatise on Geochemistry.3:293-319. https://doi.org/10.1016/b0-08-043751-6/03158-3
      Straub, S.M., Zellmer, G.F., Gómez-Tuena, A., et al., 2014.A Genetic Link between Silicic Slab Components and Calc-Alkaline Arc Volcanism in Central Mexico.Geological Society, London, Special Publications, 385(1):31-64. https://doi.org/10.1144/sp385.14
      Tatsumi, Y., Eggins, S., 1995.Subduction Zone Magmatism.Blackwell Science, Oxford, 211.
      Valley, J.W., Kinny, P.D., Schulze, D.J., et al., 1998.Zircon Megacrysts from Kimberlite:Oxygen Isotope Variability among Mantle Melts.Contributions to Mineralogy and Petrology, 133(1-2):1-11. https://doi.org/10.1007/s004100050432
      Wang, Y., Zhao, Z.F., Zheng, Y.F., et al., 2011.Geochemical Constraints on the Nature of Mantle Source for Cenozoic Continental Basalts in East-Central China.Lithos, 125(3-4):940-955. doi: 10.1016/j.lithos.2011.05.007
      Xu, S.T., Su, W., Liu., Y.C., et al., 1992.Diamond from the Dabie Shan Metamorphic Rocks and Its Implication for Tectonic Setting.Science, 256(5053):80-82. https://doi.org/10.1126/science.256.5053.80
      Xu, Z., Zhao, Z.F., Zheng, Y.F., 2012.Slab-Mantle Interaction for Thinning of Cratonic Lithospheric Mantle in North China:Geochemical Evidence from Cenozoic Continental Basalts in Central Shandong.Lithos, 146-147:202-217. https://doi.org/10.1016/j.lithos.2012.05.019
      Xu, Z., Zheng, Y.F., 2017.Continental Basalts Record the Crust-Mantle Interaction in Oceanic Subduction Channel:A Geochemical Case Study from Eastern China.Journal of Asian Earth Sciences, 145:233-259. https://doi.org/10.1016/j.jseaes.2017.03.010
      Yang, Q.L., Zhao, Z.F., Zheng, Y.F., 2012a.Modification of Subcontinental Lithospheric Mantle above Continental Subduction Zone:Constraints from Geochemistry of Mesozoic Gabbroic Rocks in Southeastern North China.Lithos, 146-147:164-182. https://doi.org/10.1016/j.lithos.2012.05.005
      Yang, Q.L., Zhao, Z.F., Zheng, Y.F., 2012b.Slab-Mantle Interaction in Continental Subduction Channel:Geochemical Evidence from Mesozoic Gabbroic Intrusives in Southeastern North China.Lithos, 155:442-460. https://doi.org/10.1016/j.lithos.2012.10.003
      Zhang, J., Zhao, Z.F., Zheng, Y.F., et al., 2010.Postcollisional Magmatism:Geochemical Constraints on the Petrogenesis of Mesozoic Granitoids in the Sulu Orogen, China.Lithos, 119(3):512-536. https://doi.org/10.1016/j.lithos.2010.08.005.
      Zhang, J., Zhao, Z.F., Zheng, Y.F., et al., 2012.Zircon Hf-O Isotope and Whole-Rock Geochemical Constraints on Origin of Postcollisional Mafic to Felsic Dykes in the Sulu Orogen.Lithos, 136-139:225-245. https://doi.org/10.1016/j.lithos.2011.06.006
      Zhang, J.J., Zheng, Y.F., Zhao, Z.F., 2009.Geochemical Evidence for Interaction between Oceanic Crust and Lithospheric Mantle in the Origin of Cenozoic Continental Basalts in East-Central China.Lithos, 110(1-4):305-326. https://doi.org/10.1016/j.lithos.2009.01.006
      Zhao, Z.F., Dai, L.Q., Zheng, Y.F., 2013.Postcollisional Mafic Igneous Rocks Record Crust-Mantle Interaction during Continental Deep Subduction.Scientific Reports, 3:3413. https://doi.org/10.1038/srep03413
      Zhao, Z.F., Dai, L.Q., Zheng, Y.F., 2015.Two Types of the Crust-Mantle Interaction in Continental Subduction Zones.Science China:Earth Sciences, 45(7):900-915(in Chinese). http://www.cnki.com.cn/Article/CJFDTOTAL-JDXG201508004.htm
      Zhao, Z.F., Liu, Z.B., Chen, Q., 2017b.Melting of Subducted Continental Crust:Geochemical Evidence from Mesozoic Granitoids in the Dabie-Sulu Orogenic Belt, East-Central China.Journal of Asian Earth Sciences, 145:260-277. https://doi.org/10.1016/j.jseaes.2017.03.038
      Zhao, Z.F., Zheng, Y.F., 2009.Remelting of Subducted Continental Lithosphere:Petrogenesis of Mesozoic Magmatic Rocks in the Dabie-Sulu Orogenic Belt.Science in China:Earth Science, 52(9):1295-1318. https://doi.org/10.1007/s11430-009-0134-8
      Zhao, Z.F., Zheng, Y.F., Chen, Y.X., et al., 2017a.Partial Melting of Subducted Continental Crust:Geochemical Evidence from Synexhumation Granite in the Sulu Orogen.GSA Bulletin, 129(11-12):1692-1707. https://doi.org/10.1130/b31675.1
      Zhao, Z.F., Zheng, Y.F., Zhang, J., et al., 2012.Syn-Exhumation Magmatism during Continental Collision:Evidence from Alkaline Intrusives of Triassic Age in the Sulu Oroge.Chemical Geology, 328:70-88. https://doi.org/10.1016/j.chemgeo.2011.11.002
      Zheng, Y.F., 2012.Metamorphic Chemical Geodynamics in Continental Subduction Zones.Chemical Geology, 328:5-48. https://doi.org/10.1016/j.chemgeo.2012.02.005
      Zheng, Y.F., 2019.Subduction Zone Geochemistry.Geoscience Frontiers, 10:1223-1254. https://doi.org/10.1016/j.gsf.2019.02.003
      Zheng, Y.F., Chen, R.X., Xu, Z., et al., 2016.The Transport of Water in Subduction Zones.Science China:Earth Sciences, 59(4):651-682. https://doi.org/10.1007/s11430-015-5258-4
      Zheng, Y.F., Chen, R.X., Zhao, Z.F., 2009.Chemical Geodynamics of Continental Subduction-Zone Metamorphism:Insights from Studies of the Chinese Continental Scientific Drilling (CCSD) Core Samples.Tectonophysics, 475(2):327-358. https://doi.org/10.1016/j.tecto.2008.09.014
      Zheng, Y.F., Chen, Y.X., 2016.Continental versus Oceanic Subduction Zones.National Science Review, 3:495-519. https://doi.org/10.1093/nsr/nww049
      Zheng, Y.F., Chen, Y.X., Dai, L.Q., et al., 2015.Developing Plate Tectonics Theory from Oceanic Subduction Zones to Collisional Orogens.Science China:Earth Sciences, 58(7):1045-1069. https://doi.org/10.1007/s11430-015-5097-3
      Zheng, Y.F., Fu, B., Gong, B., et al., 2003.Stable Isotope Geochemistry of Ultrahigh Pressure Metamorphic Rocks from the Dabie-Sulu Orogen in China:Implications for Geodynamics and Fluid Regime.Earth-Science Reviews, 62(1-2):105-161. https://doi.org/10.1016/s0012-8252(02)00133-2
      Zheng, Y.F., Hermann, J., 2014.Geochemistry of Continental Subduction-Zone Fluids.Earth, Planets and Space, 66(1):93. https://doi.org/10.1186/1880-5981-66-93
      Zheng, Y.F., Xia, Q.X., Chen, R.X., et al., 2011.Partial Melting, Fluid Supercriticality and Element Mobility in Ultrahigh-Pressure Metamorphic Rocks during Continental Collision.Earth-Science Reviews, 107(3-4):342-374. https://doi.org/10.1016/j.earscirev.2011.04.004
      Zheng, Y.F., Xu, Z., Zhao, Z.F., et al., 2018.Mesozoic Mafic Magmatism in North China:Implications for Thinning and Destruction of Cratonic Lithosphere.Science China:Earth Sciences, 61(4):353-385. https://doi.org/10.1007/s11430-017-9160-3
      Zheng, Y.F., Zhao, Z.F., 2017.Introduction to the Structures and Processes of Subduction Zones.Journal of Asian Earth Sciences, 145:1-15. https://doi.org/10.1016/j.jseaes.2017.06.034
      Zheng, Y.F., Zhao, Z.F., Chen, R.X., 2019.Ultrahigh-Pressure Metamorphic Rocks in the Dabie-Sulu Orogenic Belt:Compositional Inheritance and Metamorphic Modification.Geological Society, London, Special Publications, 474(1):89-132. doi: 10.1144/SP474.9
      Zindler, A., Hart, S., 1986.Chemical Geodynamics.Annual Review of Earth and Planetary Sciences, 14:493-571. https://doi.org/10.1146/annurev.ea.14.050186.002425
      赵子福, 戴立群, 郑永飞, 2015.大陆俯冲带两类壳幔相互作用.中国科学:地球科学, 45(7):900-915. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkx-cd201507002
    • 加载中
    图(3)
    计量
    • 文章访问数:  4743
    • HTML全文浏览量:  1804
    • PDF下载量:  161
    • 被引次数: 0
    出版历程
    • 收稿日期:  2019-09-02
    • 刊出日期:  2019-12-15

    目录

      /

      返回文章
      返回