Melt transfer and migration occurs through both supra-and sub-solidus rocks. Mechanisms
of melt transfer include dyking, mobile hydrofracturing and diffuse porous melt flow where …

4.1 Introduction 51 4.2 Elastic constants 52 4.3 Isothermal versus adiabatic elastic constants
55 4.4 Experimental techniques 57 4.5 Some general trends in elasticity: Birch's law 59 4.6 …

Results from a thermal‐mechanical model (HT1) that includes midcrustal channel flow are
compatible with many features of the Himalayan‐Tibetan system. Radioactive self‐heating …

Simple shear deformation experiments on three‐phase, hydrous, haplogranitic magmas,
composed of quartz crystals (24–65 vol.%), CO2‐rich gas bubbles (9–12 vol.%) and melt in …

The evolution of melt segregation in deforming partially molten olivine-rich rocks has been
studied in a series of laboratory experiments. During deformation, melt segregates into …

We present the results of two-dimensional numerical modelling experiments on the thermal
evolution of Archean greenstones as they sink into a less dense, hot and weak felsic crust …

The rheology of volatile-bearing crystal mushes was constrained by deformation
experiments on hydrous (2.52 wt.% H2O) haplogranitic magmas containing quartz crystals …

Partial melting significantly weakens crustal rocks by introducing a low‐viscosity liquid
phase. However, near‐concomitant melt drainage can remove this weak phase, potentially …

Crustal flow is an important tectonic process active in continent‐continent collisions and
which may be significant in the development of convergent plate boundaries. In this study …

The physics of magmatic systems within continental crust is poorly understood. We
developed a thermomechanical compositional two-phase flow formulation based on the …