Software for teleseismic body wave modeling through stacks of anisotropic layers
The structure of the Earth's crust and upper mantle gives useful information on the internal composition and dynamics of our planet. Some of the most widely used techniques to infer these properties are based on examining the effect of teleseismic body wave (i.e., P and S waves that originate from distant earthquakes and arrive as plane waves) propagation (e.g., transmission and scattering) through stratified media. Modeling the seismic response from stacks of subsurface layers is therefore an essential tool in characterizing their effect on observed seismograms.
This package contains
fortran modules to synthesize teleseismic
body-wave propagation through stacks of generally anisotropic and strictly horizontal
layers using the matrix propagator approach of Kennett (1983), as implemented
in Thomson (1997).
The software also properly models reverberations from an overlying column of water using the R/T
matrix expressions of Bostock and Trehu (2012),
effectively simulating ocean-bottom seismic (OBS) station recordings. The software
will be useful in a variety of teleseismic receiver-based studies, such as P or S
receiver functions, long-period P-wave polarization, shear-wave splitting from
core-refracted shear waves (i.e., SKS, SKKS), etc. It may also be the starting point
for stochastic inverse methods (e.g., Monte Carlo sampling). The main part of the
code is written in
python wrappers. Common computational
workflows are covered in the Jupyter notebooks bundled with this package.
Installation, Usage, API documentation and Jupyter Notebooks are described at https://paudetseis.github.io/Telewavesim/
If you use
Telewavesim in your work, please cite the Zenodo DOI
and the following paper:
- Audet, P., Thomson, C.J., Bostock, M.G., and Eulenfeld, T. (2019). Telewavesim: Python software for teleseismic body wave modeling. Journal of Open Source Software, 4(44), 1818, https://doi.org/10.21105/joss.01818
All constructive contributions are welcome, e.g. bug reports, discussions or suggestions for new features. You can either open an issue on GitHub or make a pull request with your proposed changes. Before making a pull request, check if there is a corresponding issue opened and reference it in the pull request. If there isn't one, it is recommended to open one with your rationale for the change. New functionality or significant changes to the code that alter its behavior should come with corresponding tests and documentation. If you are new to contributing, you can open a work-in-progress pull request and have it iteratively reviewed.
Examples of straightforward contributions include adding more elastic constants or notebooks that describe published examples of teleseismic body-wave modeling. Suggestions for improvements (speed, accuracy, etc.) are also welcome.
Bostock, M.G., and Trehu, A.M. (2012). Wave-field decomposition of ocean-bottom seismograms. Bulletin of the Seismological Society of America, 102, 1681-1692. https://doi.org/10.1785/0120110162
Kennett, B.L.N. (1983). Seismic wave propagation in stratified media. Cambridge University Press, 342pp. https://www.oapen.org/search?identifier=459524
Thomson, C.J. (1997). Modelling surface waves in anisotropic structures: I. Theory. Physics of the Earth and Planetary interiors, 103, 195-206. https://doi.org/10.1016/S0031-9201(97)00033-2