Projects

This link will take you to the SCEC website which hosts the 1D/diffused 2D steady-state geotherm model code used in Shinevar et al. (2018).

This MATLAB toolbox allows for the interpretation of mantle seismic wave speed in terms of composition and temperature. See Shinevar et al. (2022) for more details!

Lower crustal rheology is important to understand crustal deformation and post-seismic stress transfer for earthuqakes, vital to better understand earthquake risk in tectonically active regions! Lower crustal rheology is dependent on many parameters: temperature, pressure, strain rate/stress, mineral assemblage/whole-rock composition, water content, and grain size!

The linked github repository includes a finite-difference multi-component garnet diffusion model for a radially symmetric sphere using the garnet diffusivities from Chu and Ague (2015) used in Shinevar et al. (2021).