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Evidence for anisotropy in the super-thick sedimentary basin, Bay of Bengal

  • James N. Brune
  • Govardhan Mekala
  • Yuehua Zeng
Rapid Communication

Abstract

Evidence for anisotropy in the super-thick sedimentary basin under the northern Bay of Bengal is presented. Surface wave group velocity data given by Brune and Singh (1986) is better fit by an anisotropic model than an isotropic one. This lends support to the hypothesis that the mid-crustal rocks are metasediments and that the section of sediments and metasediments is more than 20 km thick.

Keywords

Bay of Bengal sedimentary basins anisotropy 

References

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Copyright information

© Indian Academy of Sciences 1995

Authors and Affiliations

  • James N. Brune
    • 1
  • Govardhan Mekala
    • 1
  • Yuehua Zeng
    • 1
  1. 1.Seismological LaboratoryUniversity of NevadaRenoUSA

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