An Introduction to Seismology, Earthquakes, and Earth Structure

By C. Thurber. 2003

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Earthquake triggering and large-scale geologic storage of carbon dioxide (2012, unknown): “2 uses well-established seismological relationships to show how the magnitude of an earthquake is related to the size of the fault that slipped and the amount of fault slip that occurred (16).”
An arbitrary high-order discontinuous Galerkin method for elastic waves on unstructured meshes - IV. Anisotropy (2007, background): “The most general linear elastic stress-strain relation can be expressed through a tensorial constitutive law (Hooke’s Law), see e.g. (Stein & Wysession 2003), of the form σij = cijklεkl (1) The entries of the fourth-order elasticity tensor cijkl can be reduced to 21 independent real coefficients in…”