AxiSEM

AxiSEM is a parallel spectral-element method for 3D (an-)elastic, anisotropic and acoustic wave propagation in spherical domains. It requires axisymmetric background models and runs within a 2D computational domain, thereby reaching all desired highest observable frequencies (up to 2Hz) in global seismology. The Fortran2003 (OpenMP, MPI) code scales very well on supercomputers and is available under the GPL license. For more details see the website at www.axisem.info.

SEISMOLOGYAxiSEM

Contributor(s)

Initial contribute: 2019-07-02

Classification(s)

Application-focused categoriesNatural-perspectiveSolid-earth regions

Detailed Description

English {{currentDetailLanguage}} English

Quoted from: https://geodynamics.org/cig/software/axisem/ 

AxiSEM is a parallel spectral-element method for 3D (an-)elastic, anisotropic and acoustic wave propagation in spherical domains. It requires axisymmetric background models and runs within a 2D computational domain, thereby reaching all desired highest observable frequencies (up to 2Hz) in global seismology. The Fortran2003 (OpenMP, MPI) code scales very well on supercomputers and is available under the GPL license. For more details see the website at www.axisem.info.

Please see our corresponding paper "AxiSEM: broadband 3-D seismic wavefields in axisymmetric media" published in Solid Earth, 5, 425-445, doi:10.5194/se-5-425-2014, 2014. Please cite this paper (and others) when using AxiSEM.

User Manual

The AxiSEM user manual is available online.

Community Wiki

Visit the AxiSEM Wiki page for additional support with building, using, or modifying AxiSEM.

AxiSEM Publications List

Research publications using AxiSEM.

Community Discussion

Browse the CIG Mailing List Archive to find past discussions and previous troubleshooting help, or post to the CIG forum with questions or comments.

模型元数据

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Yue Songshan (2019). AxiSEM, Model Item, OpenGMS, https://geomodeling.njnu.edu.cn/modelItem/8d6e93f5-a1ec-45d3-904d-29d96b922fcc
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Contributor(s)

Initial contribute : 2019-07-02

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