Experimental dissolution‐precipitation creep in quartz aggregates at high temperatures

Geophysical Research Letters

Volumn 18, Issue 8, 1991, Pages 1401-1404

  Cox, S F ^a   Paterson, M S ^a  

^a AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

Author keywords

[No Author keywords available]

Indexed keywords

AGGREGATE; COMPACTION CREEP; DEFORMATION PROCESS; DISSOLUTION; HIGH TEMPERATURE; PRECIPITATION; QUARTZ;

EID: 0026304482     PISSN: 00948276     EISSN: 19448007     Source Type: Journal    
DOI: 10.1029/91GL01802     Document Type: Article

References (17)

1. The solubility of quartz in supercritical water
2. Coupled grain‐scale dilatancy and mass transfer during deformation at high fluid pressures: examples from Mt Lyell, Tasmania
3. Pressure solution experiments on quartz sand
4. High fluid pressures during regional metamorphism and deformation: implications for mass transport and deformation mechanisms
5. Experimental pressure solution‐deposition on quartz grains: the crucial effect of the nature of the fluid
6. Diffusional crack healing in calcite: The influence of crack geometry upon healing rate
7. Interface healing in synthetic marbles: an SEM/TEM study, Eos
8. Surface and interfacial free energies of quartz
9. A high temperature high pressure apparatus for rock deformation
10. Nonhydrostatic thermodynamics and its geologic applications
11. Creep in polycrystalline aggregates by matter transport through a liquid phase
12. Experimental investigation of pressure solution of quartz
13. The kinetics of rock deformation by pressure solution
14. Pressure solution in theory, nature and experiment
15. Destruction of porosity through pressure solution
16. Fluids in the lithosphere, 1. Experimentally‐determined wetting characteristics of CO2‐H2O fluids and their implications for fluid transport, host‐rock physical properties, and fluid inclusion formation