Articles

DEVELOPMENT OF STUDIES OF PLUME, SUPERPLUME AND THEIR ORIGIN

  • ZHOU Wen-ge ,
  • XIE Hong-sen ,
  • HOU Wei
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  • Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002,China

Received date: 2004-11-02

  Revised date: 2005-06-13

  Online published: 2005-10-25

Abstract

In the last thirties years great advances of the studies of mantle plumes have been made. Based on the depth of origin, the mantle plumes have been subdivided into three groups. These are deep plume, transition zone origin plume and uppermantle plume. In this paper the criteria used to diagnose deep plumes and transition zone origin plumes are induced. The distribution of these plumes around the Earth surface and their shape are described. In addition, the superplumes in lower mantle and ultra-low velocity zones in mostly lower mantle found by the investigation of seismic tomography give an important evidence for the origin of plumes.

Cite this article

ZHOU Wen-ge , XIE Hong-sen , HOU Wei . DEVELOPMENT OF STUDIES OF PLUME, SUPERPLUME AND THEIR ORIGIN[J]. Advances in Earth Science, 2005 , 20(10) : 1095 -1099 . DOI: 10.11867/j.issn.1001-8166.2005.10.1095

References

[1] Xie Hongsen. An Introduction to Material Science in the Earth’s Interior [M].Beijing: Science Press, 1997. 173,227-229,278-284.[谢鸿森.地球深部物质科学导论[M].北京:科学出版社,1997. 173,227-229,278-284.]
[2] Richard A K. Plume from the core lost and found[J].Science, 2003, 299:35-36.
[3] Courtillot V, Davaille A, Besse J,et al. Three distinct types of hotspots in the Earth's mantle[J].Earth and Planetary Science Letters, 2003,205:295-308.
[4] Nataf H C. Seismic imaging of mantle plumes[J].Annual Review Earth Planetary Sciences,2000, 28: 391-417.
[5] Richard A K. From Earth's core to African oil[J].Science, 2001, 294:287.
[6] Chinese Map Press,ed. World Atlas[M].Beijing: Chinese Map Press, 2003. [中国地图出版社编制.世界地图集[M].北京:中国地图出版社,2003.] 
[7] Tackley P. Mantle convection and plate tectonics:Toward an integrated physical and chemical theory[J].Science, 2000, 288:2 002-2 007.
[8] Manga M. Shaken, not stirred[J]. Nature,2001,410:1 041-1 043.
[9] Montagner J P, Ritsema J. Interactions between ridges and plumes[J].Science, 2001, 294:1 472-1 473.
[10] Garnero E J. Heterogeneity of the lowermost mantle[J].Annual Review Earth Planetary Sciences, 2000, 28:509-537.
[11] Williams Q, Revenaugh J, Garnero E. A correlation between ultra-low basal velocities in the mantle and hot spots[J].Science,1998, 281:546-549.
[12] Panning M, Romanowicz B. Inference on flow at the base of Earth's mantle based on seismic anisotropy[J].Science,2004,303:351-353.
[13] Romanowicz B, Gung Y. Superplumes from the core-mantle boundary to the lithosphere: Implications for heat flux[J].Science, 2002, 296:513-516.
[14] Keken P E V, Hauri E H, Ballentine C J. Mantle mixing: The generation, preservation, and destruction of chemical heterogegeity[J].Annual Review Earth Planetary Sciences,2002, 30:493-525.
[15] Ni S, Tan Eh, Gurnis M,et al. Sharp sides to the African superplume[J].Science, 2002, 296:1 850-1 852.
[16] Zhao D. Global tomographic images of mantle plumes and subducting slabs:Insight into deep Earth dynamics[J].Physics of The Earth and Planetary Interiors, 2004, 146:3-34.
[17] Schubert G, Masters G, Olson P, et al. Superplumes or plume clusters?[J].Physics of the Earth and Planetary Interiors, 2004, 146:147-162.

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