Do coeval mafic and felsic magmas in post-collisional to within-plate regimes necessarily imply two contrasting, mantle and crustal, sources? A review

Granitic magma transport by fracture propagation

The generation, segregation, ascent and emplacement of granite magma: the migmatite-to-crustally-derived granite connection in thickened orogens

Tensor Analysis for Physicists. By J.A. Schouten. Second edition. Pp. xii, 277. 30s. 1954. (Geoffrey Cumberlege, Oxford University Press.)

Partial melting of mafic (amphibolitic) lower crust by periodic influx of basaltic magma

An integral equation approach to diffusion

Green's function for the vector wave equation in a mildly heterogeneous continuum

Procedures are discussed for obtaining Green's functions for potential problems in heterogeneous materials. Such fundamental solutions are required in the boundary element method. An exact funddamental solution for a linearly varying, layered two dimensional potential problem is given that does not appear to be available elsewhere.

Green's functions for heterogeneous media potential problems

Fundamental Green's functions are developed for a class of heterogeneous materials for Helmholtz and Laplace equations. Although limited to specific heterogeneities, the resulting Green's functions are particularly simple and may be used directly in standard boundary integral equation methods.

Green’s Functions for Helmholtz and Laplace Equations in Heterogeneous Media

Harmonic wave propagation through viscoelastic heterogeneous media exhibiting mild stochasticity — I. Fundamental solutions

Richard Paul Shaw

Papers

An integral equation approach to diffusion

Green's function for the vector wave equation in a mildly heterogeneous continuum

Green's functions for heterogeneous media potential problems

Green’s Functions for Helmholtz and Laplace Equations in Heterogeneous Media

Harmonic wave propagation through viscoelastic heterogeneous media exhibiting mild stochasticity — I. Fundamental solutions