四海龙湾玛珥湖沉积物中碱流质火山灰的来源及其意义

郭正府 刘嘉麒 樊祺诚 贺怀宇 隋淑珍 储国强 刘强 J.F.W.Negendank. 四海龙湾玛珥湖沉积物中碱流质火山灰的来源及其意义[J]. 岩石学报, 2005, 21(1): 251-255.
引用本文: 郭正府 刘嘉麒 樊祺诚 贺怀宇 隋淑珍 储国强 刘强 J.F.W.Negendank. 四海龙湾玛珥湖沉积物中碱流质火山灰的来源及其意义[J]. 岩石学报, 2005, 21(1): 251-255.
GUO ZhengFu,LIU JiaQi,FAN QiCheng,HE HuaiYu,SUI ShuZhen,CHU GuoQiang,LIU Qiang and J. F. W. Negendank Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China Institute of Geology,China Seismological Bureau,Beijing 100029,China GeoForschungsZentrum,Potsdam D-144473,Germany. Source of volcanic ash in the sediments of Sihailongwan maar lake, NE China, and its significance[J]. Acta Petrologica Sinica, 2005, 21(1): 251-255.
Citation: GUO ZhengFu,LIU JiaQi,FAN QiCheng,HE HuaiYu,SUI ShuZhen,CHU GuoQiang,LIU Qiang and J. F. W. Negendank Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China Institute of Geology,China Seismological Bureau,Beijing 100029,China GeoForschungsZentrum,Potsdam D-144473,Germany. Source of volcanic ash in the sediments of Sihailongwan maar lake, NE China, and its significance[J]. Acta Petrologica Sinica, 2005, 21(1): 251-255.

四海龙湾玛珥湖沉积物中碱流质火山灰的来源及其意义

  • 基金项目:

    国家自然科学基金项目(批准号:40072026和40372045)资助

  • 四海龙湾玛珥湖位于东北新生代龙岗火山区内,在玛珥湖沉积物距湖底69-70cm处分离出新鲜的火山灰,根据火山灰产出的层位、原生沉积特征、形貌和碱流质化学成分特征,属于长白山天池火山公元1199-1200年大喷发的产物,这一结果不仅表明天池火山历史时期大喷发的规模比原来估计的还要大,并且为建立千年以来四海龙湾沉积物及古气候演化的时间标尺提供了依据。
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  • [1]

    Acharyya S K, Basu P K. 1993. Toba ash on the Indian subcontinent and its implications for correlation of Late Pleistocene alluvium. Quaternary Research, 40: 10 - 19.

    [2]

    Brauer A. 1994. Weiehselzeitliche sediments des Holzmaaresarvenchronologie und Nachweis yon Klimaschwankungen. Dokumenta natirae, 85: 1 -210.

    [3]

    Cui Z X, Jin Y T, Li N. 2000. A historical record of 1199/1200 AD eruption of Tianchi volcano, Changbai mountains and its significance, Acta Petrologiea Sinica, 16 (2): 191 - 193 (in Chinese with English abstract).

    [4]

    Fan Q C, Liu R X, Wei H Q, Sui J L, Li Ni. 1999. Petrology and Geochemistry of volcanic rocks erupted from active volcanoes of Jinlongdingzi, Longgang volcanic field, NE China, Acta Petrologica Sinica, 15(4) :584 -589 (in Chinese with English abstract).

    [5]

    Gill J, Dunlap C, McCurry M. 1992. Large-volume, mid-latitude, C1rich eruption during 600 ~ 1000 AD, Baitoushan, China. Chapman Conference on Climate, Volcanism and Global Change, AGU, March 23-27, Hito, Hawaii, 1-10.

    [6]

    Guo Z F, Liu J Q, Sui S Z, Liu Q, He H Y, Ni Y Y. 2001. Estimation of amount of volatiles released from Baitoushan volcanoes, Changbai mountains, NE China and its significances. Sciences in China (Series D), 31 (8) :668 - 676 ( in Chinese).

    [7]

    Guo Z F, Liu J Q, Chu G Q, Negendank J F W. 2002. Composition and origin of tephra of the Huguangyan maar lake. Quaternary Sciences,22 (3) :266 -272 (in Chinese with English abstract).

    [8]

    Hall V A, Pilcher J R. 2002. Late-Quaternary Icelandic tephras in Ireland and Great Britain: detection, characterization and usefulness. The Holocene, 12 (2): 223 -230.

    [9]

    Horn S, Schmincke H. -U. 2000. Volatile emission during the eruption of Baitoushan volcano (China/North Korea) ca. 969 AD. Bull.Volcanol. , 61:537 -555.

    [10]

    Liu J Q. 1999. Volcanoes in China. Beijing: Science Press, 13 - 126 (in Chinese).

    [11]

    Liu R X, Wei H Q, Li J T, et al. Tianchi volcano in Changbai mountains. In: Liu R X (ed), Volcanism and human environment.Beijing: Seismological Press, 1995. 1 - 13 (in Chinese with English abstract).

    [12]

    Liu R X, Wei H Q, Li J T. Eruptions of Tianchi volcano in Changbai mountains. Beijing: Science Press, 1998. 83 - 107 (in Chinese with English abstract).

    [13]

    Machida H, Arai F. Extensive ash falls in and around the Sea of Japan from large late Quaternary eruptions. J. Volcanol. Geothermal. Res,1983, 18:151-164.

    [14]

    Mingram J, Schettler G, Allen J, et al. The Eifel of N. E. -China-maar and crater lakes of the Long Gang Volcanic Field. Terra Nostra,2000, 6: 353 - 363.

    [15]

    Pilcher J R, Hall V A, McCormac F G. 1996. An outline tephrochronology for the Holocene of the north of Ireland. Journal of Quaternary Science, 11 (6): 485 - 494.

    [16]

    Rose W I, Chesner C A. 1987. Dispersal of ash in the great Toba eruption, 75 ka. Geology, 15:913-917.

    [17]

    Sigurdsson, H. 2000. Encyclopedia of Volcanoes, New York: Academic Press, 1 - 1384.

    [18]

    Sarna-Wojcicki A M, Davis J O. 1991. Quaternary tephrochronology. In: Morrison R B ed. Quaternary nonglacial geology. Boulder, Colorado:The Geological Society of America, 93 - 116.

    [19]

    Sui S Z, Liu J Q, Guo Z F, Hall V A, Turney C S M, Wang W Y.2003. Extraction and measuring techniques of volcanic ash. Earth Science Frontiers, 10 (1): 111 - 116 (in Chinese with English abstract).

    [20]

    Usinger. 1991. Ein Stechbohrgerat Zum Bergen von torfen und Seesedinenten fur Einsatz biszu grosseren Tiefen. In: Symposium of Paleolimnology of Maar lakes ( Eds. Zolitschka B and Negendank J F W). Bitburg, 55.

    [21]

    Zielinski G A, Mayewski P A, Meeker L D. 1994. Record of volcanism since 7000 B. C. from the GISP2 Greenland Ice Core and implications for the volcano-climate system. Science, 264:948 -952.

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出版历程
修回日期:  2004-04-28
刊出日期:  2005-01-31

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