华北克拉通岩石圈地幔的锂同位素特征与熔体改造作用
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摘要
华北克拉通是显生宙以来全球古老克拉通破坏最为剧烈的地区。华北克拉通破坏及其相关的科学问题引起了国内外地质学家的广泛关注。有关华北克拉通破坏的研究已取得了许多重要进展,使我们认识到其破坏不仅表现为岩石圈厚度的剧烈减薄,更重要的是岩石圈地幔的物质组成与性质发生了巨大转变,即从古生代克拉通型转变为新生代大洋型。本文在综述华北地幔捕虏体锂同位素地球化学特征的基础上,进一步揭示了华北岩石圈地幔高度不均一的组成特征,以及不同来源的熔体对岩石圈地幔的改造作用,为深入认识华北岩石圈地幔的转变过程提供进一步的制约。
The North China Craton is the most strongly destructed region of ancient cratons in the world since the Phanerozoic era. The destruction of North China Craton and its related scientific issues have attracted extensive attention of geoscientists at home and abroad. Much important progresses have been made in the study of the destruction of North China Craton. It is recognized that the destruction of North China Craton is not only reflected by the severe thinning of the lithosphere beneath North China Craton, more importantly, but also reflected by the huge transformation of component and property of the lithospheric mantle, from the Paleozoic cratonic type to Cenozoic oceanic type. On the basis of summarizing the geochemical characteristics of lithium isotopes of mantle xenoliths in the North China Craton, this paper has further revealed the highly inhomogeneous feature for compositions of the lithospheric mantle beneath the craton and the modification of lithospheric mantle by variously sourced melts, and has provided further constraint for understanding the transformation process of the lithospheric mantle beneath the craton.
The North China Craton is the most strongly destructed region of ancient cratons in the world since the Phanerozoic era. The destruction of North China Craton and its related scientific issues have attracted extensive attention of geoscientists at home and abroad. Much important progresses have been made in the study of the destruction of North China Craton. It is recognized that the destruction of North China Craton is not only reflected by the severe thinning of the lithosphere beneath North China Craton, more importantly, but also reflected by the huge transformation of component and property of the lithospheric mantle, from the Paleozoic cratonic type to Cenozoic oceanic type. On the basis of summarizing the geochemical characteristics of lithium isotopes of mantle xenoliths in the North China Craton, this paper has further revealed the highly inhomogeneous feature for compositions of the lithospheric mantle beneath the craton and the modification of lithospheric mantle by variously sourced melts, and has provided further constraint for understanding the transformation process of the lithospheric mantle beneath the craton.
引文
Aulbach S, Rudnick R L. 2009. Origins of non-equilibrium lithium isotopic fractionation in xenolithic peridotite minerals: Examples from Tanzania. Chemical Geology, 258(1-2): 17-27
Eggins S M, Rudnick R L, McDonough W F. 1998. The composition of peridotites and their minerals: A laser-ablation ICP-MS study. Earth and Planetary Science Letters, 154(1-4): 53-71
Elliott T, Jeffcoate A, Bouman C. 2004. The terrestrial Li isotope cycle: Light-weight constraints on mantle convection. Earth and Planetary Science Letters, 220(3-4): 231-245
Elliott T, Thomas A, Jeffcoate A, Niu Y L. 2006. Lithium isotope evidence for subduction-enriched mantle in the source of mid-ocean-ridge basalts. Nature, 443(7111): 565-568
Fan W M, Menzies M A. 1992. Destruction of aged lower lithosphere and accretion of asthenosphere mantle beneath eastern China. Geotectonica et Metallogenia, 16(2): 171-180
Fan W M, Zhang H F, Baker J, Jarvis K E, Mason P R D, Menzies M A. 2000. On and off the north China craton: Where is the Archaean keel? Journal of Petrology, 41(7): 933-950
Griffin W L, O'Reilly S Y, Ryan C G. 1992. Composition and thermal structure of the lithosphere beneath South Africa, Siberia and China: Proton microprobe studies. International Symposium on Cenozoic Volcanic Rocks and Deep-seated Xenoliths of China and Its Environs. Beijing: Science Press, 65-66
Liu D Y, Nutman A P, Compston W, Wu J S, Shen Q H. 1992. Remnants of ≥ 3800 Ma crust in the Chinese part of the Sino-Korean craton. Geology, 20(4): 339-342
Menzies M A, Fan W M, Zhang M. 1993. Palaeozoic and Cenozoic lithoprobes and the loss of >120 km of Archaean lithosphere, Sino-Korean craton, China. In: Prichard H M, Alabaster T, Harris N B W, Neary C R, eds. Magmatic Processes and Plate Tectonics. Geological Society of London, Special Publication, 71-81
Pearson D G. 1999. The age of continental roots. Lithos, 48(1-4): 171-194
Seitz H M, Brey G P, Lahaye Y, Durali S, Weyer S. 2004. Lithium isotopic signatures of peridotite xenoliths and isotopic fractionation at high temperature between olivine and pyroxenes. Chemical Geology, 212(1-2): 163-177
Seitz H M, Woodland A B. 2000. The distribution of lithium in peridotitic and pyroxenitic mantle lithologies - an indicator of magmatic and metasomatic processes. Chemical Geolology, 166, 47-64
Su B X, Zhang H F, Deloule E, Sakyi P A, Xiao Y, Tang Y J, Hu Y, Ying J F, Liu P P. 2012. Extremely high Li and low δ7Li signatures in the lithospheric mantle. Chemical Geology, 292-293, 149-157
Su B X, Zhang H F, Deloule E, Vigier N, Hu Y, Tang Y J, Xiao Y, Sakyi P A. 2014. Distinguishing silicate and carbonatite mantle metasomatism by using lithium and its isotopes. Chemical Geology, 381: 67-77
Tang Y J, Zhang H F, Nakamura E, Moriguti T, Kobayashi K, Ying J F. 2007a. Lithium isotopic systematics of peridotite xenoliths from Hannuoba, North China Craton: Implications for melt-rock interaction in the considerably thinned lithospheric mantle. Geochimica et Cosmochimica Acta, 71(17): 4327-4341
Tang Y J, Zhang H F, Ying J F. 2007b. Review of the lithium isotope system as a geochemical tracer. International Geology Review, 49(4): 374-388
Tang Y J, Zhang H F, Ying J F, Zhang J, Liu X M. 2008. Refertilization of ancient lithospheric mantle beneath the central North China Craton: Evidence from petrology and geochemistry of peridotite xenoliths. Lithos, 101(3-4): 435-452
Tang Y J, Zhang H F, Ying J F. 2010. A brief review of isotopically light Li-a feature of the enriched mantle? International Geology Review, 52(9): 964-976
Tang Y J, Zhang H F, Nakamura E, Ying J F. 2011. Multistage melt/fluid-peridotite interactions in the refertilized lithospheric mantle beneath the North China Craton: Constraints from the Li-Sr-Nd isotopic disequilibrium between minerals of peridotite xenoliths. Contributions to Mineralogy and Petrology, 161(6): 845-861
Tang Y J, Zhang H F, Deloule E, Su B X, Ying J F, Xiao Y, Hu Y. 2012. Slab-derived lithium isotopic signatures in mantle xenoliths from northeastern North China Craton. Lithos, 149: 79-90
Tang Y J, Zhang H F, Santosh M, Ying J F. 2013a. Differential destruction of the North China Craton: A tectonic perspective. Journal of Asian Earth Sciences, 78: 71-82
Tang Y J, Zhang H F, Ying J F, Su B X. 2013b. Widespread refertilization of cratonic and circum-cratonic lithospheric mantle. Earth-Science Reviews, 118: 45-68
Tang Y J, Zhang H F, Ying J F, Su B X, Chu Z Y, Xiao Y, Zhao X M. 2013c. Highly heterogeneous lithospheric mantle beneath the Central Zone of the North China Craton evolved from Archean mantle through diverse melt refertilization. Gondwana Research, 23(1): 130-140
Tang Y J, Zhang H F, Deloule E, Su B X, Ying J F, Santosh M, Xiao Y. 2014. Abnormal lithium isotope composition from the ancient lithospheric mantle beneath the North China Craton. Scientific Reports, 4: 4274
Teng F Z, Rudnick R L, McDonough W F, Gao S, Tomascak P B, Liu Y S. 2008. Lithium isotopic composition and concentration of the deep continental crust. Chemical Geology, 255(1-2): 47-59
Tomascak P B, Langmuir C H, le Roux P J, Shirey S B. 2008. Lithium isotopes in global mid-ocean ridge basalts. Geochimica et Cosmochimica Acta, 72(6): 1626-1637
Woodland A B, Seitz H M, Yaxley G M. 2004. Varying behaviour of Li in metasomatised spinel peridotite xenoliths from western Victoria, Australia. Lithos, 75(1-2): 55-66
Wunder B, Meixner A, Romer R L, Feenstra A, Schettler G, Heinrich W. 2007. Lithium isotope fractionation between Li-bearing staurolite, Li-mica and aqueous fluids: An experimental study. Chemical Geology, 238(3-4): 277-290
Xiao Y, Zhang H F, Deloule E, Su B X, Tang Y J, Sakyi P A, Hu Y, Ying J F. 2015. Large Lithium Isotopic Variations in Minerals from Peridotite Xenoliths from the Eastern North China Craton. The Journal of Geology, 123(1): 79-94
Xu R, Liu Y S, Tong X R, Hu Z C, Zong K Q, Gao S. 2013. In-situ trace elements and Li and Sr isotopes in peridotite xenoliths from Kuandian, North China Craton: Insights into Pacific slab subduction-related mantle modification. Chemical Geology, 354: 107-123
Zack T, Tomascak P B, Rudnick R L, Dalpé C, McDonough W F. 2003. Extremely light Li in orogenic eclogites: The role of isotope fractionation during dehydration in subducted oceanic crust. Earth and Planetary Science Letters, 208(3-4): 279-290
Zhang H F, Deloule E, Tang Y J, Ying J F. 2010. Melt/rock interaction in remains of refertilized Archean lithospheric mantle in Jiaodong Peninsula, North China Craton: Li isotopic evidence. Contributions to Mineralogy and Petrology, 160(2): 261-277
Zhang H F, Goldstein S, Zhou X H, Sun M, Zheng J P, Cai Y. 2008. Evolution of subcontinental lithospheric mantle beneath eastern China: Re-Os isotopic evidence from mantle xenoliths in Paleozoic kimberlites and Mesozoic basalts. Contributions to Mineralogy and Petrology, 155(3): 271-293
Zhao G C, Sun M, Wilde S A, Li S Z. 2005. Late Archean to Paleoproterozoic evolution of the North China Craton: Key issues revisited. Precambrian Research, 136(2): 177-202
Zheng J P, O'Reilly S Y, Griffin W L, Lu F X, Zhang M, Pearson N J. 2001. Relict refractory mantle beneath the eastern North China block: Significance for lithosphere evolution. Lithos, 57(1): 43-66
黄方. 2011. 高温下非传统稳定同位素分馏. 岩石学报, 27(2): 365-382
李佩, 夏群科, Deloule E. 2012. 山东蓬莱新生代岩石圈地幔的异常锂同位素组成: 橄榄岩包体的离子探针分析. 高校地质学报, 18(1): 62-73
苏本勋. 2017. 锂同位素在地幔地球化学中的应用. 矿物岩石地球化学通报, 36(1): 6-13
汤艳杰, 张宏福, 英基丰. 2011. 地幔中EM1端员成因的锂同位素制约. 矿物岩石地球化学通报, 30(1): 11-17
万红琼, 孙贺, 刘海洋, 肖益林. 2015. 俯冲带Li同位素地球化学: 回顾与展望. 地学前缘, 22(5): 29-43
肖益林, 孙贺, 顾海欧, 黄建, 李王晔, 刘磊. 2015. 大陆深俯冲过程中的熔/流体成分与地球化学分异. 中国科学(D辑), 45(8): 1063-1087
张宏福. 2009. 橄榄岩-熔体相互作用: 克拉通型岩石圈地幔能够被破坏之关键. 科学通报, 54(14): 2008-2026
张宏福, 汤艳杰, 赵新苗, 杨岳衡. 2007. 非传统同位素体系在地幔地球化学研究中的重要性及其前景. 地学前缘, 14(2): 37-57
郑建平, 路凤香. 1999. 胶辽半岛金伯利岩中地幔捕虏体岩石学特征: 古生代岩石圈地幔及其不均一性. 岩石学报, 15(1): 65-74
朱日祥, 徐义刚, 朱光, 张宏福, 夏群科, 郑天愉. 2012. 华北克拉通破坏. 中国科学(D辑), 42(8): 1135-1159
Eggins S M, Rudnick R L, McDonough W F. 1998. The composition of peridotites and their minerals: A laser-ablation ICP-MS study. Earth and Planetary Science Letters, 154(1-4): 53-71
Elliott T, Jeffcoate A, Bouman C. 2004. The terrestrial Li isotope cycle: Light-weight constraints on mantle convection. Earth and Planetary Science Letters, 220(3-4): 231-245
Elliott T, Thomas A, Jeffcoate A, Niu Y L. 2006. Lithium isotope evidence for subduction-enriched mantle in the source of mid-ocean-ridge basalts. Nature, 443(7111): 565-568
Fan W M, Menzies M A. 1992. Destruction of aged lower lithosphere and accretion of asthenosphere mantle beneath eastern China. Geotectonica et Metallogenia, 16(2): 171-180
Fan W M, Zhang H F, Baker J, Jarvis K E, Mason P R D, Menzies M A. 2000. On and off the north China craton: Where is the Archaean keel? Journal of Petrology, 41(7): 933-950
Griffin W L, O'Reilly S Y, Ryan C G. 1992. Composition and thermal structure of the lithosphere beneath South Africa, Siberia and China: Proton microprobe studies. International Symposium on Cenozoic Volcanic Rocks and Deep-seated Xenoliths of China and Its Environs. Beijing: Science Press, 65-66
Liu D Y, Nutman A P, Compston W, Wu J S, Shen Q H. 1992. Remnants of ≥ 3800 Ma crust in the Chinese part of the Sino-Korean craton. Geology, 20(4): 339-342
Menzies M A, Fan W M, Zhang M. 1993. Palaeozoic and Cenozoic lithoprobes and the loss of >120 km of Archaean lithosphere, Sino-Korean craton, China. In: Prichard H M, Alabaster T, Harris N B W, Neary C R, eds. Magmatic Processes and Plate Tectonics. Geological Society of London, Special Publication, 71-81
Pearson D G. 1999. The age of continental roots. Lithos, 48(1-4): 171-194
Seitz H M, Brey G P, Lahaye Y, Durali S, Weyer S. 2004. Lithium isotopic signatures of peridotite xenoliths and isotopic fractionation at high temperature between olivine and pyroxenes. Chemical Geology, 212(1-2): 163-177
Seitz H M, Woodland A B. 2000. The distribution of lithium in peridotitic and pyroxenitic mantle lithologies - an indicator of magmatic and metasomatic processes. Chemical Geolology, 166, 47-64
Su B X, Zhang H F, Deloule E, Sakyi P A, Xiao Y, Tang Y J, Hu Y, Ying J F, Liu P P. 2012. Extremely high Li and low δ7Li signatures in the lithospheric mantle. Chemical Geology, 292-293, 149-157
Su B X, Zhang H F, Deloule E, Vigier N, Hu Y, Tang Y J, Xiao Y, Sakyi P A. 2014. Distinguishing silicate and carbonatite mantle metasomatism by using lithium and its isotopes. Chemical Geology, 381: 67-77
Tang Y J, Zhang H F, Nakamura E, Moriguti T, Kobayashi K, Ying J F. 2007a. Lithium isotopic systematics of peridotite xenoliths from Hannuoba, North China Craton: Implications for melt-rock interaction in the considerably thinned lithospheric mantle. Geochimica et Cosmochimica Acta, 71(17): 4327-4341
Tang Y J, Zhang H F, Ying J F. 2007b. Review of the lithium isotope system as a geochemical tracer. International Geology Review, 49(4): 374-388
Tang Y J, Zhang H F, Ying J F, Zhang J, Liu X M. 2008. Refertilization of ancient lithospheric mantle beneath the central North China Craton: Evidence from petrology and geochemistry of peridotite xenoliths. Lithos, 101(3-4): 435-452
Tang Y J, Zhang H F, Ying J F. 2010. A brief review of isotopically light Li-a feature of the enriched mantle? International Geology Review, 52(9): 964-976
Tang Y J, Zhang H F, Nakamura E, Ying J F. 2011. Multistage melt/fluid-peridotite interactions in the refertilized lithospheric mantle beneath the North China Craton: Constraints from the Li-Sr-Nd isotopic disequilibrium between minerals of peridotite xenoliths. Contributions to Mineralogy and Petrology, 161(6): 845-861
Tang Y J, Zhang H F, Deloule E, Su B X, Ying J F, Xiao Y, Hu Y. 2012. Slab-derived lithium isotopic signatures in mantle xenoliths from northeastern North China Craton. Lithos, 149: 79-90
Tang Y J, Zhang H F, Santosh M, Ying J F. 2013a. Differential destruction of the North China Craton: A tectonic perspective. Journal of Asian Earth Sciences, 78: 71-82
Tang Y J, Zhang H F, Ying J F, Su B X. 2013b. Widespread refertilization of cratonic and circum-cratonic lithospheric mantle. Earth-Science Reviews, 118: 45-68
Tang Y J, Zhang H F, Ying J F, Su B X, Chu Z Y, Xiao Y, Zhao X M. 2013c. Highly heterogeneous lithospheric mantle beneath the Central Zone of the North China Craton evolved from Archean mantle through diverse melt refertilization. Gondwana Research, 23(1): 130-140
Tang Y J, Zhang H F, Deloule E, Su B X, Ying J F, Santosh M, Xiao Y. 2014. Abnormal lithium isotope composition from the ancient lithospheric mantle beneath the North China Craton. Scientific Reports, 4: 4274
Teng F Z, Rudnick R L, McDonough W F, Gao S, Tomascak P B, Liu Y S. 2008. Lithium isotopic composition and concentration of the deep continental crust. Chemical Geology, 255(1-2): 47-59
Tomascak P B, Langmuir C H, le Roux P J, Shirey S B. 2008. Lithium isotopes in global mid-ocean ridge basalts. Geochimica et Cosmochimica Acta, 72(6): 1626-1637
Woodland A B, Seitz H M, Yaxley G M. 2004. Varying behaviour of Li in metasomatised spinel peridotite xenoliths from western Victoria, Australia. Lithos, 75(1-2): 55-66
Wunder B, Meixner A, Romer R L, Feenstra A, Schettler G, Heinrich W. 2007. Lithium isotope fractionation between Li-bearing staurolite, Li-mica and aqueous fluids: An experimental study. Chemical Geology, 238(3-4): 277-290
Xiao Y, Zhang H F, Deloule E, Su B X, Tang Y J, Sakyi P A, Hu Y, Ying J F. 2015. Large Lithium Isotopic Variations in Minerals from Peridotite Xenoliths from the Eastern North China Craton. The Journal of Geology, 123(1): 79-94
Xu R, Liu Y S, Tong X R, Hu Z C, Zong K Q, Gao S. 2013. In-situ trace elements and Li and Sr isotopes in peridotite xenoliths from Kuandian, North China Craton: Insights into Pacific slab subduction-related mantle modification. Chemical Geology, 354: 107-123
Zack T, Tomascak P B, Rudnick R L, Dalpé C, McDonough W F. 2003. Extremely light Li in orogenic eclogites: The role of isotope fractionation during dehydration in subducted oceanic crust. Earth and Planetary Science Letters, 208(3-4): 279-290
Zhang H F, Deloule E, Tang Y J, Ying J F. 2010. Melt/rock interaction in remains of refertilized Archean lithospheric mantle in Jiaodong Peninsula, North China Craton: Li isotopic evidence. Contributions to Mineralogy and Petrology, 160(2): 261-277
Zhang H F, Goldstein S, Zhou X H, Sun M, Zheng J P, Cai Y. 2008. Evolution of subcontinental lithospheric mantle beneath eastern China: Re-Os isotopic evidence from mantle xenoliths in Paleozoic kimberlites and Mesozoic basalts. Contributions to Mineralogy and Petrology, 155(3): 271-293
Zhao G C, Sun M, Wilde S A, Li S Z. 2005. Late Archean to Paleoproterozoic evolution of the North China Craton: Key issues revisited. Precambrian Research, 136(2): 177-202
Zheng J P, O'Reilly S Y, Griffin W L, Lu F X, Zhang M, Pearson N J. 2001. Relict refractory mantle beneath the eastern North China block: Significance for lithosphere evolution. Lithos, 57(1): 43-66
黄方. 2011. 高温下非传统稳定同位素分馏. 岩石学报, 27(2): 365-382
李佩, 夏群科, Deloule E. 2012. 山东蓬莱新生代岩石圈地幔的异常锂同位素组成: 橄榄岩包体的离子探针分析. 高校地质学报, 18(1): 62-73
苏本勋. 2017. 锂同位素在地幔地球化学中的应用. 矿物岩石地球化学通报, 36(1): 6-13
汤艳杰, 张宏福, 英基丰. 2011. 地幔中EM1端员成因的锂同位素制约. 矿物岩石地球化学通报, 30(1): 11-17
万红琼, 孙贺, 刘海洋, 肖益林. 2015. 俯冲带Li同位素地球化学: 回顾与展望. 地学前缘, 22(5): 29-43
肖益林, 孙贺, 顾海欧, 黄建, 李王晔, 刘磊. 2015. 大陆深俯冲过程中的熔/流体成分与地球化学分异. 中国科学(D辑), 45(8): 1063-1087
张宏福. 2009. 橄榄岩-熔体相互作用: 克拉通型岩石圈地幔能够被破坏之关键. 科学通报, 54(14): 2008-2026
张宏福, 汤艳杰, 赵新苗, 杨岳衡. 2007. 非传统同位素体系在地幔地球化学研究中的重要性及其前景. 地学前缘, 14(2): 37-57
郑建平, 路凤香. 1999. 胶辽半岛金伯利岩中地幔捕虏体岩石学特征: 古生代岩石圈地幔及其不均一性. 岩石学报, 15(1): 65-74
朱日祥, 徐义刚, 朱光, 张宏福, 夏群科, 郑天愉. 2012. 华北克拉通破坏. 中国科学(D辑), 42(8): 1135-1159