Effect of partial melting on rock deformation: Experimental and natural evidences on rocks of granitic compositions
- 1 October 1981
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 78 (1-4) , 545-565
- https://doi.org/10.1016/0040-1951(81)90028-7
Abstract
No abstract availableThis publication has 14 references indexed in Scilit:
- Experimental deformation of partially melted granitic rocks at 600–900° C and 250 MPa confining pressureTectonophysics, 1980
- Stress Relaxation in CrystalsPhysica Status Solidi (b), 1979
- The effect of high temperature and high confining pressure on compressional wave velocities in quartz-bearing and quartz-free igneous and metamorphic rocksTectonophysics, 1978
- Critical phenomena in the rheology of partially melted rocksTectonophysics, 1978
- The effect of cracks on the thermal expansion of rocksEarth and Planetary Science Letters, 1977
- Dilatancy and the Strength of Rocks containing Pore Water under Undrained ConditionsGeophysical Journal International, 1976
- The production of granitic melts during ultrametamorphismContributions to Mineralogy and Petrology, 1970
- Thermodynamic Properties of Water to 1,000° C and 10,000 BarsPublished by Geological Society of America ,1969
- Dilatancy in the fracture of crystalline rocksJournal of Geophysical Research, 1966
- Dependence of Mechanical Strength of Brittle Polycrystalline Specimens on Porosity and Grain SizeJournal of the American Ceramic Society, 1959