Large scale three-dimensional boundary element simulation of subduction. We present a novel approach for modeling subduction using a Multipole-accelerated Boundary Element Method (BEM). The present approach allows large-scale modeling with a reduced number of elements and scales linearly with the problem size. For the first time the BEM has been applied to a subduction model in a spherical planet with an upper-lower mantle discontinuity, in conjunction with a free-surface mesh algorithm.
References in zbMATH (referenced in 1 article )
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- Quevedo, L.; Hansra, B.; Morra, G.; Butterworth, N.; Müller, R.D.: Oblique mid ocean ridge subduction modelling with the parallel fast multipole boundary element method (2013)