The experimental deformation of flint, a water-rich (1-2 wt%) fine-grained (1 Ixm) microcrystalline quartz, has been studied using a gas-confining medium apparatus at 300 MPa confining pressure in the temperature range 500-1000 ~ In constant strainrate axial compression tests a mechanically unstable behaviour with peaked and undulating stress-strain curves, especially at the faster strain rates, is manifest. The rheology of these tests can be approximately described by the traditional power-law equation with a stress exponent (n) of between 3 and 5, and an apparent activation energy (Q) of 108 kJ mo1-1. However, the strain-independent ('steady-state') equation is only a partial description of the data. The mechanical properties were studied at lower stresses using stress relaxation testing, this method has the advantage of recording specimen response over a very small strain interval (c. 1%), i.e. nearly constant structure. These tests revealed that in a high stress regime above 100 MPa the rheology was only weakly dependent on strain and very similar to the constant strain-rate behaviour. Below 100 MPa the rheology can be described by a power law with Q = 64 kJ mol-l and n = 1. The low-stress behaviour is extremely sensitive to specimen strain, the strain rate decreasing with increasing strain for a given stress.The optical microstructure reveals that the mechanical instabilities are related to localized displacement zones, sometimes en echelon, consisting of relatively large grains (10 ~m). The important reduction of the integral infrared absorption of deformed specimens, a 98% reduction of the initial water content, suggests that a pore fluid was developed by specimen dehydration in the sealed (undrained) assembly. The presence of pores or bubbles decorating grain boundaries and microfractures normal to the piston-specimen interface both testify to the presence of the pore fluid during deformation. The pore fluid pressure may have approached the confining pressure resulting in a near-zero effective pressure. Transmission electron microscopy revealed the presence of many Brazil micro-twins parallel to grain boundaries. The twins are thought to be growth defects indicating rapid grain growth during deformation. Dislocations in the basal plane were observed with a 1/3 (a)-type Burgers vector. Dislocations were also observed in the grain boundaries, possibly caused by grain-boundary sliding in the low stress regime.The complete lattice preferred orientation (LPO) of homogeneously deformed specimens has been determined by X-ray texture goniometry. The inverse pole figures have a strong concentration of compression axes parallel, and a weaker concentration normal, to the c-axis. The local c-axis pole figures in heterogeneously deformed specimens were characterized by the photometric technique. The c-axis pole figures in the bulk are identical to that determined by X-rays in homogeneously deformed specimens. In the displacement zones the fabrics are asymmetric with respect to the zone boundaries. The asymmetry is not...