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Moho面和上地幔间断面大尺度地形起伏的低阶球谐分析

  • 何小波 ,
  • 周蕙兰
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  • 中国科学院研究生院计算地球动力学重点实验室, 北京 100049

收稿日期: 2004-07-29

  修回日期: 2004-12-28

  网络出版日期: 2005-05-15

基金资助

国家自然科学基金(40374009;40234047)资助

The Low Degree Spherical Harmonic Analysis on the Large Scale Topographies of the Moho and the Upper Mantle Discontinuities

  • HE Xiao-Bo ,
  • ZHOU Hui-Lan
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  • Laboratory of Computational Geodynamics, Graduate School of the Chinese Academy of Sciences, Beijing 100049, China

Received date: 2004-07-29

  Revised date: 2004-12-28

  Online published: 2005-05-15

摘要

对全球地形高程和Moho面深度(CRUST20模型)及上地幔各间断面深度数据进行了球谐分析.在此基础上,通过叠加前4阶模式得到了各类数据的空间大尺度分布信息,通过叠加振幅平方值最大的4项得到了各类数据的空间主能量分布.结果表明,Moho面和‘410’间断面的地形存在半球尺度的大尺度非对称性,而且南北半球非对称性比东西半球的更显著;而‘520’和‘660’间断面的地形起伏已没有半球尺度那么大的非对称性,而是尺度略小些的不对称性.

本文引用格式

何小波 , 周蕙兰 . Moho面和上地幔间断面大尺度地形起伏的低阶球谐分析[J]. 中国科学院大学学报, 2005 , 22(3) : 315 -321 . DOI: 10.7523/j.issn.2095-6134.2005.3.009

Abstract

In this paper, the global topography, the depth of the Moho(the cxustalmodel CRUST2.0),th a depths ofupper mantle discontinuities were analyzed using the spherical harmonics. Based on these data, the spatial large scaledistribution information has been obtained by sacking the first 4 degree modes, and the main energy distributionshave been understood by synthesizing the four items with the maxunal squares of amplitudes. The results show thatthere exiss a large scale asynrrnetry on the scale of semisphere in the topographies of the Moho and the‘410'discontinuities, and the asynrrnetry character of the nor-tl}rsouth semispheres is more obvious than that of the westeast semispheres; However, there exiss a scale asymmetry on the small side in the topographies of‘520' and‘660'discontinu ides, instead of such a large sphere scale asynrrnetry.

参考文献

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[1] 马宗晋, 宋晓东, 杜品仁, 等. 地球南北半球的非对称性. 地球物理学报, 2002, 45(1) : 26~ 32

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[3] 黄立人, 马宗晋, 朱建新. 地球非对称变形的最新观测证据. 地震学报, 2002, 24(2) : 196~ 199

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