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    中国东部上地幔岩石相转变及其意义

    樊祺诚 隋建立

    樊祺诚, 隋建立, 2009. 中国东部上地幔岩石相转变及其意义. 地球科学, 34(3): 387-391.
    引用本文: 樊祺诚, 隋建立, 2009. 中国东部上地幔岩石相转变及其意义. 地球科学, 34(3): 387-391.
    FAN Qi-cheng, SUI Jian-li, 2009. Phase Transition of Upper Mantle Rock in Eastern China and Its Significance. Earth Science, 34(3): 387-391.
    Citation: FAN Qi-cheng, SUI Jian-li, 2009. Phase Transition of Upper Mantle Rock in Eastern China and Its Significance. Earth Science, 34(3): 387-391.

    中国东部上地幔岩石相转变及其意义

    基金项目: 

    国家自然科学基金项目 40772038

    详细信息
      作者简介:

      樊祺诚(1948-), 男, 研究员, 主要从事火山与地球内部物质研究.E-mail: fqc@ies.ac.cn

    • 中图分类号: P583

    Phase Transition of Upper Mantle Rock in Eastern China and Its Significance

    • 摘要: 中国东部新生代玄武岩和大别-苏鲁超高压变质带中的含石榴石相橄榄岩, 带来了发生在上地幔的尖晶石→石榴石相转变和铝辉石→贫铝辉石+石榴石的重要信息, 为中国东部上地幔岩石结构分层奠定了重要基础.通过岩石学与实验岩石学的研究, 推导出发生相转变的P-T条件, 为建立中国东部大陆上地幔岩石分层结构提供了重要约束.尖晶石二辉橄榄岩向石榴石二辉橄榄岩相转变发生在55~70km, 随着深度增加, 石榴石二辉橄榄岩从富铝石榴石二辉橄榄岩(70~120km) 转变为贫铝石榴石二辉橄榄岩(> 120~150km).

       

    • 表  1  中国东部新生代玄武岩中代表性尖晶石/石榴石二辉橄榄岩矿物化学成分(%)

      Table  1.   Mineral compositions of representative spinel/garnet lherzolite in Cenozoic basalts from eastern China (%)

      表  2  中国东部新生代玄武岩中代表性石榴石二辉橄榄岩矿物化学成分(%)

      Table  2.   Mineral compositions of representative garnet lherzolite in Cenozoic basalts from eastern China (%)

      表  3  中国东部新生代玄武岩中含石榴石相橄榄岩P-T平衡条件

      Table  3.   P-T estimation for garnet-bearing peridotites in Cenozoic basalts from eastern China

      表  4  大别-苏鲁超高压变质带超镁铁岩辉石矿物化学成分(%)

      Table  4.   Pyroxene compositions of ultramafic rocks from Dabie-Sulu ultrahigh-presure metamorphic belt (%)

    • Ave Lallemant, H. G., Mercier, J. C. C., Carter, J. L., et al., 1980. Rheology of the upper mantle: Inferences from peridotite xenoliths. Tectono physics, 70: 85-113. doi: 10.1016/0040-1951(80)90022-0
      Cao, R. L., Zhu, S. H., 1990. Sanidine-olivine-diopside mantle metasomatic association found in a garnet lherzolite xenolith from Xilong, Zhejiang Province. In: Professional committee for mantle mineralogy, petrology and geochemistry under China Society of Mineralogy, Petrology and Geochemistry, ed., Collected papers on uppermantle characteristics and dynamics of China. Seismological Publishing House, Beijing, 34-44 (in Chinese).
      Carswell, D.A., 1986. The metamorphic evolution of Mg-Cr type Norwegian garnet peridotites. Lithos, 19(3-4): 279-297. doi: 10.1016/0024-4937(86)90028-9
      Chi, J. S., 1988. Study on Cenozoic basalt and upper mantle in China (with special concern to kinberlite). China University of Geosciences Press, Beijing (in Chinese).
      Dawson, J. B., 1980. Kimberlites and their xenoliths. Springer-Verlag, Berlin, Heidelberg, New York.
      E, M. L., Zhao, D. S., 1987. Cenozoic basalt and xenolith from depth in China. Science Press, Beijing (inChinese).
      Fan, Q. C., Hooper, P. R., 1989. The mineral chemistry of ultramafic xenoliths of eastern China: Implications for upper mantle composition and the paleogeotherms. J. Petrology, 30 (5): 1117-1158. doi: 10.1093/petrology/30.5.1117
      Fan, Q. C., Liu, R. X., 1990. Study on phase transition of multiple spinel-garnet peridotites in upper mantle beneath eastern China. In: Professional committee for mantle mineralogy, petrology and geochemistry under China Society of Mineralogy, Petrology and Geochemistry, ed., Collected papers on upper mantle characteristics and dynamics of China. Seismological Publishing House, Beijing, 72-82 (in Chinese).
      Fan, Q. C., Liu, R. X., 1994. Spinel-garnet lherzolite in Late Tertiary li mburgitic pipe from Hebi, Henan Provinceand its genesis. In: Ouyang, Z. Y., ed., New progress in mineralogy, petrology and geochemistry study in China. Lanzhou University Press, Lanzhou, 141-142 (inChinese).
      Fan, Q. C., Liu, R. X., Xie, H. S., et al., 1997a. Experi mental study of spinel-garnet phase transitionin uppermantle and its significance. Science in China (Ser. D), 40 (4): 383-389. doi: 10.1007/BF02877569
      Fan, Q. C., Liu, R. X., Xie, H. S., et al., 1997b. Ultrahigh pressure (4.5-5.5GPa) experimental research on pyroxene-garnet transition and its significance. Chinese Science Bulletin, 42 (17): 1456-1459. doi: 10.1007/BF02883058
      Fan, Q. C., Liu, R. X., Ma, B. L., 1992. Preli minary study on high-pressure metamorphism of unltramafic rocks in North Jiangsu-South Shandong region. Acta Petrologica Sinica, 8 (1): 90-96 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB199201008.htm
      Fan, Q. C., Liu, R. X., Ma, B. L., et al., 1996a. The petrolith and ultrahigh-pressure metamorphism of Maowu maficunltramafic rock block in Dabieshan Mountains. Acta Petrologica Sinica, 12 (1): 29-47 (in Chinese withEnglish abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB601.002.htm
      Fan, Q. C., Liu, R. X., Zhang, Q., et al., 1996b. The petrology and high pressure minernal assemblage of mafic-ultramafic rocks in ultrahigh pressure zone of Dabieshan Mountains. Sciencein China (Ser. D), 39 (3): 329-336.
      Fan, Q. C., Sui, J. L., Zhao, Y. W., et al., 2008. Preliminary study on garnet peridotite xenolith of Quaternary volcanic rocks in middle Daxing'an Mountain range. Acta Petrologica Sinica, 24 (11): 2563-2568 (in Chinesewith English abstract).
      Jin, S. Y., Pan, S. A., 1998. Mantle-derived xenoliths of spinel-garnet lherzolite from Nushan and their implications for petro-physics. Earth Science——Journal of ChinaUniversity of Geosciences, 23 (5): 475-479 (in Chinesewith English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX805.007.htm
      Lallement, H. L., Mercier, H. G., Carter, J. C., et al., 1980. Rheology of upper mantle: Inferences from peridotite xenoliths. Tectonophysics, 70 (1-2): 85-113. doi: 10.1016/0040-1951(80)90022-0
      Liu, R. X., Yang, M. E., Xu, H. J., et al., 1981. Preliminary study of ultramafic xenoliths from Cenozoic alkaline basalts in North China. Seismological Geology, 3 (3): 1-16, 4 (4): 39-48 (in Chinese with English abstract).
      MacGregor, I. D., 1970. The effect of CaO, Cr2O3, Fe2O3 and Al2O3 on the stability of spinel and garnet peridotites. Phys. Earth Planet. Interiors, 3: 372-377. doi: 10.1016/0031-9201(70)90077-4
      Nickel, K. G., Green, D. H., 1985. Expirical geothermobarometry for garnet peridotites andi mplications for thenature of the lithosphere, kimberlite and diamonds. Earth Planet. Sci. Lett. , 73 (1): 158-170. doi: 10.1016/0012-821X(85)90043-3
      O'Neil, H. S. C., 1981. The transition between lherzolite and garnet lherzolite, and its use as a geobarmeter. Contrib. Miner. Petrol. , 77: 185-194. doi: 10.1007/BF00636522
      Ringwood, A. E., 1967. The pyroxene-garnet transformation in the earth's mantle. Earth Planet. Sci. Lett. , 2 (3): 255-263. doi: 10.1016/0012-821X(67)90138-0
      Wells, P. R. A., 1977. Pyroxenethermometry in simple andcomplex systems. Contr. Miner. Petrol. , 62 (2): 129-139. doi: 10.1007/BF00372872
      Xu, Y. G., Lin, C. Y., Shi, L. B., et al., 1995. Upper mantle geotherm for eastern China and its geological implications. Science in China (Ser. B), 38 (12): 1482-1492. http://qikan.cqvip.com/Qikan/Article/Detail?id=3001276475
      曹荣龙, 朱寿华, 1990. 浙江西垄石榴石二辉橄榄岩包体中发现的透长石-橄榄石-透辉石地幔交代组合. 见: 中国矿物岩石地球化学学会地幔矿物岩石地球化学专业委员会主编, 中国上地幔特征与动力学论文集. 北京: 地震出版社, 34-44.
      池际尚, 1988. 中国东部新生代玄武岩及上地幔研究(附金伯利岩). 北京: 中国地质大学出版社.
      鄂莫岚, 赵大升, 1987. 中国东部新生代玄武岩及深源岩石包体. 北京: 科学出版社.
      樊祺诚, 刘若新, 1990. 上地幔尖晶石-石榴石复合橄榄岩与相转变. 见: 中国矿物岩石地球化学学会地幔矿物岩石地球化学专业委员会主编, 中国上地幔特征与动力学论文集. 北京: 地震出版社, 72-82.
      樊祺诚, 刘若新, 1994. 河南鹤壁晚第三纪玻基辉橄岩筒中尖晶石/石榴石二辉橄榄岩及成因. 见: 欧阳自远编, 中国矿物学岩石学地球化学研究新进展. 兰州: 兰州大学出版社, 141-142.
      樊祺诚, 刘若新, 马宝林, 1992. 苏北-胶南高压变质超镁铁岩的初步研究. 岩石学报, 1: 90-96. doi: 10.3321/j.issn:1000-0569.1992.01.009
      樊祺诚, 刘若新, 马宝林, 等, 1996. 大别山毛屋超高压变质镁铁-超镁铁的原岩与变质作用. 岩石学报, 12 (1): 29-47. doi: 10.3321/j.issn:1000-0569.1996.01.003
      樊祺诚, 隋建立, 赵勇伟, 等, 2008. 大兴安岭中部第四纪火山岩中石榴石橄榄岩捕虏体的初步研究. 岩石学报, 24 (11): 2563-2568. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200811011.htm
      金淑燕, 潘顺安, 1998. 女山玄武岩中尖晶石-石榴石二辉橄榄岩包体及其岩石物理意义. 地球科学————中国地质大学学报, 23 (5): 475-479. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX805.007.htm
      刘若新, 杨美娥, 胥怀济, 等, 1981. 华北新生代碱性玄武岩中超镁铁质捕虏体的初步研究. 地震地质, 3 (3): 1-16, 4 (4): 39-48.
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    • 收稿日期:  2009-01-12
    • 刊出日期:  2009-05-25

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