• 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

    岩浆作用与地球深部过程

    莫宣学

    莫宣学, 2019. 岩浆作用与地球深部过程. 地球科学, 44(5): 1487-1493. doi: 10.3799/dqkx.2019.972
    引用本文: 莫宣学, 2019. 岩浆作用与地球深部过程. 地球科学, 44(5): 1487-1493. doi: 10.3799/dqkx.2019.972
    Mo Xuanxue, 2019. Magmatism and Deep Geological Process. Earth Science, 44(5): 1487-1493. doi: 10.3799/dqkx.2019.972
    Citation: Mo Xuanxue, 2019. Magmatism and Deep Geological Process. Earth Science, 44(5): 1487-1493. doi: 10.3799/dqkx.2019.972

    岩浆作用与地球深部过程

    doi: 10.3799/dqkx.2019.972
    详细信息
      作者简介:

      莫宣学(1938-), 男, 教授, 中国科学院院士, 学科专业为岩石学, 研究方向为岩浆-构造-成矿

    • 中图分类号: P54

    Magmatism and Deep Geological Process

    • 摘要: 为纪念马杏垣院士诞辰一百周年而作.首先简述了地球系统科学的基本思想和指导意义.指出岩浆作用实质上是地球各层圈之间相互作用的结果,岩浆是地球各层圈之间物质和能量交换的重要载体.通过众多研究实例,重点讨论了岩浆作用的地球动力学意义:一方面,火成岩及其所携带的深源岩石包体可以当作地球深部的"探针"和"窗口";另一方面,火成岩也是大地构造事件的记录,可以用以恢复古板块构造格局,追溯大地构造演化历史.

       

    • [1] Aitchison, J.C., Ali, J.R., Davis, A.M., 2007.When and Where did India and Asia Collide?.Journal of Geophysical Research, 112(B5):B05423. https://doi.org/10.1029/2006jb004706
      [2] Best, M.G., 2003.Igneous and Metamorphic Petrology (2nd Edition).Oxford Blackwell Science, Oxford.
      [3] Carmichael, I.S.E., Turner, F.J., Verhoogen, J., 1974.Igneous Petrology.McGraw-Hill Company, New York.
      [4] Christiansen, E.H., Hamblin, W.K., 2014.Dynamic Earth.Jones & Bartlett Learning, Burlington.
      [5] Condie, K.C., 1997.Plate Tectonics and Crustal Evolution (4th Edition).Butterworth-Heinemann, Oxford.
      [6] Condie, K.C., 2005.Earth as an Evolving Planetary System.Elsevier Academic Press, New York.
      [7] Defant, M.J., Drummond, M.S., 1990.Derivation of Some Modern Arc Magmas by Melting of Young Subducted Lithosphere.Nature, 347(6294):662-665. https://doi.org/10.1038/347662a0
      [8] Deng, J.F., Luo, Z.H., Su, S.G., et al., 2004.Ptrogeneses, Tectonic Environments and Mineralization.Geological Publishing House, Beijing, 1-381(in Chinese).
      [9] Deng, J.F., Mo, X.X., Zhao, H.L., et al., 2004.A New Model for the Dynamic Evolution of Chinese Lithosphere:'Continental Roots-Plume Tectonics'.Earth-Science Reviews, 65(3-4):223-275. https://doi.org/10.1016/j.earscirev.2003.08.001
      [10] Ding, L., Kapp, P., Wan, X.Q., 2005.Paleocene-Eocene Record of Ophiolite Obduction and Initial India-Asia Collision, South Central Tibet.Tectonics, 24(3):1-18. https://doi.org/10.1029/2004tc001729
      [11] Hou, Z.Q., Cook, N.J., 2009.Metallogenesis of the Tibetan Collisional Orogen:A Review and Introduction to the Special Issue.Ore Geology Reviews, 36(1-3):2-24. https://doi.org/10.1016/j.oregeorev.2009.05.001
      [12] Hou, Z.Q., Duan, L.F., Lu, Y.J., et al., 2015.Lithospheric Architecture of the Lhasa Terrane and Its Control on Ore Deposits in the Himalayan-Tibetan Orogen.Economic Geology, 110(6):1541-1575. https://doi.org/10.2113/econgeo.110.6.1541
      [13] Jaeger, J.J., Courtillot, V., Tapponnier, P., 1989.Paleontological View of the Ages of the Deccan Traps, the Cretaceous/Tertiary Boundary, and the India-Asia Collision.Geology, 17(4):316.https://doi.org/10.1130/0091-7613(1989)017<0316:pvotao>2.3.co;2 doi: 10.1130/0091-7613(1989)017<0316:pvotao>2.3.co;2
      [14] Kump, L., 2004.The Earth System (2nd Editon).Prentice Hall, New Jersey.
      [15] Mo, X.X., 2011.Magma and Magmatic/Igneous Rocks:A Lithoprobe into the Deep Earth and Records of the Earth's Evolution.Chinese Journal of Nature, 33(5):255-259, 313(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZRZZ201105003.htm
      [16] Mo, X.X., 2018.Earth Deep Process and Mineralization.Chinese High Science and Technology, 32:1-3(in Chinese). http://d.old.wanfangdata.com.cn/Periodical/xddz201704006
      [17] Mo, X.X., Dong, G.C., Zhao, Z.D., et al., 2005.Spatial and Temporal Distribution and Characteristics of Granitoids in the Gangdese, Tibet and Implication for Crustal Growth and Evolution.Geological Journal of China Universities, 11(3):281-290(in Chinese with English abstract).
      [18] Mo, X.X., Dong, G.C., Zhao, Z.D., et al., 2005.Timing of Magma Mixing in the Gangdisê Magmatic Belt during the India-Asia Collision:Zircon SHRIMP U-Pb Dating.Acta Geologica Sinica (English Edition), 79(1):66-76. https://doi.org/10.1111/j.1755-6724.2005.tb00868.x
      [19] Mo, X.X., Hou, Z.Q., Niu, Y.L., et al., 2007.Mantle Contributions to Crustal Thickening during Continental Collision:Evidence from Cenozoic Igneous Rocks in Southern Tibet.Lithos, 96(1-2):225-242. https://doi.org/10.1016/j.lithos.2006.10.005
      [20] Mo, X.X., Lu, F.X., Shen, S.Y., et al., 1993.Sanjiang Tethyan Volcanism and Mineralization.Geological Publishing House, Beijing, 1-267(in Chinese with English abstract).
      [21] Mo, X.X., Niu, Y.L., Dong, G.C., et al., 2008.Contribution of Syncollisional Felsic Magmatism to Continental Crust Growth:A Case Study of the Paleogene Linzizong Volcanic Succession in Southern Tibet.Chemical Geology, 250(1-4):49-67. https://doi.org/10.1016/j.chemgeo.2008.02.003
      [22] Mo, X.X., Zhao, Z.D., Deng, J.F., et al., 2003.Response of Volcanism to the India-Asia Collision.Earth Science Frontiers, 10(3):135-148(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200303019.htm
      [23] Mo, X.X., Zhao, Z.D., Deng, J.F., et al., 2006.Petrology and Geochemistry of Postcollisional Volcanic Rocks from the Tibetan Plateau:Implications for Lithosphere Heterogeneity and Collision-Induced Asthenospheric Mantle Flow.Geological Society of America Special Paper, 409:507-530. https://pubs.geoscienceworld.org/books/book/583/chapter/3803900/Petrology-and-geochemistry-of-postcollisional
      [24] Mo, X.X., Zhao, Z.D., Yu, X.H., et al., 2009.Cenozoic Collisional-Postcollisional Igneous Rocks in the Tibetan Plateau.Geological Publishing House, Beijing, 1-396(in Chinese with English abstract).
      [25] Mo, X.X., Zhao, Z.D., Zhou, S., et al., 2002.Evidence for Timing of the Initiation of India-Asia Collision from Igneous Rocks in Tibet.EOS Trans.AGU, 83(47):F10003. http://adsabs.harvard.edu/abs/2002AGUFM.S62B1201M
      [26] 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
      [27] Stanley, S.M., 2005.Earth System History.W.H.Freeman, San Francisco.
      [28] Wan, X.Q., Jansa, L.F., Sarti, M., 2002.Cretaceous and Paleogene Boundary Strata in Southern Tibet and Their Implication for the India-Eurasia Collision.Lethaia, 35(2):131-146. https://doi.org/10.1080/002411602320183999
      [29] Wilson, M., 1989.Igneous Petrogenesis: A Global Tectonic Approach.Chapman & Hall, London.
      [30] Wyllie, P.J., 1976.The Way the Earth Works:An Introduction to the New Global Geology and Its Revolutionary Development.The Journal of Geology, 84(4):502-502. https://doi.org/10.1086/628222
      [31] Wyllie, P.J., Osmaston, M.F., Morrison, M.A., 1984.Constraints Imposed by Experimental Petrology on Possible and Impossible Magma Sources and Products (and Discussion).Philosophical Transactions of the Royal Society A:Mathematical, Physical and Engineering Sciences, 310(1514):439-456. https://doi.org/10.1098/rsta.1984.0003
      [32] Yin, A., Harrison, T.M., 2000.Geologic Evolution of the Himalayan-Tibetan Orogen.Annual Review of Earth and Planetary Sciences, 28(1):211-280. https://doi.org/10.1146/annurev.earth.28.1.211
      [33] Zhang, S.Q., Mahoney, J.J., Mo, X.X., et al., 2005.Evidence for a Widespread Tethyan Upper Mantle with Indian-Ocean-Type Isotopic Characteristics.Journal of Petrology, 46(4):829-858. https://doi.org/10.1093/petrology/egi002
      [34] Zhao, Z.D., Mo, X.X., Dilek, Y., et al., 2009.Geochemical and Sr-Nd-Pb-O Isotopic Compositions of the Post-Collisional Ultrapotassic Magmatism in SW Tibet:Petrogenesis and Implications for India Intra-Continental Subduction beneath Southern Tibet.Lithos, 113(1-2):190-212. https://doi.org/10.1016/j.lithos.2009.02.004
      [35] Zhao, Z.D., Mo, X.X., Sun, C.G.et al., 2008.Mantle Xenoliths in Southern Tibet:Geochemistry and Constraints for the Nature of the Mantle.Acta Petrologica Sinica, 24(2):193-202.
      [36] Zhou, S., Mo, X.X., Dong, G.C., et al., 2004.40Ar-39Ar Geochronology of Cenozoic Linzizong Volcanic Rocks from Linzhou Basin, Tibet, China, and Their Geological Implications.Chinese Science Bulletin, 49(18):1970-1979. https://doi.org/10.1007/bf03184291
      [37] Zhou, S., Mo, X.X., Dong, G.C., et al., 2004.40Ar-39Ar Geochronology of Cenozoic Linzizong Volcanic Rocks from Linzhou Basin, Tibet, China, and Their Geological Implications.Chinese Science Bulletin, 49(20):2095-2103(in Chinese). http://www.cnki.com.cn/Article/CJFDTotal-JXTW200418014.htm
      [38] Zhu, D.C., Zhao, Z.D., Niu, Y.L., et al., 2011.The Lhasa Terrane:Record of a Microcontinent and Its Histories of Drift and Growth.Earth and Planetary Science Letters, 301(1-2):241-255. https://doi.org/10.1016/j.epsl.2010.11.005
      [39] 邓晋福, 罗照华, 苏尚国, 等, 2004.岩石成因、构造环境与成矿作用.北京:地质出版社, 1-381.
      [40] 莫宣学, 2011.岩浆与岩浆岩:地球深部"探针"与演化记录.自然杂志, 33(5):255-259, 313. http://d.old.wanfangdata.com.cn/Periodical/zrzz201105002
      [41] 莫宣学, 2018.地球深部过程与成矿作用.中国高科技期刊, 32:1-3. http://cdmd.cnki.com.cn/Article/CDMD-10183-2007018959.htm
      [42] 莫宣学, 董国臣, 赵志丹, 等, 2005.西藏冈底斯带花岗岩的时空分布特征及地壳生长演化信息.高校地质学报, 11(3):281-290. doi: 10.3969/j.issn.1006-7493.2005.03.001
      [43] 莫宣学, 路凤香, 沈上越, 等, 1993.三江特提斯火山作用与成矿.北京:地质出版社, 1-26.
      [44] 莫宣学, 赵志丹, 邓晋福, 等, 2003.印度-亚洲大陆主碰撞过程的火山作用响应.地学前缘, 10(3):135-148. doi: 10.3321/j.issn:1005-2321.2003.03.013
      [45] 莫宣学, 赵志丹, 喻学惠, 等, 2009.青藏高原新生代碰撞-后碰撞火成岩.北京:地质出版社, 1-396.
      [46] 周肃, 莫宣学, 董国臣, 等, 2004.西藏林周盆地林子宗火山岩40Ar-39Ar年代格架.科学通报49(20):2095-2103. doi: 10.3321/j.issn:0023-074X.2004.20.014
    • 加载中
    计量
    • 文章访问数:  5860
    • HTML全文浏览量:  2919
    • PDF下载量:  1066
    • 被引次数: 0
    出版历程
    • 刊出日期:  2019-05-15

    目录

      /

      返回文章
      返回