Effect of microcracking on pressure-solution strain rate: the Gratz grain-boundary model

Geology

Volumn 26, Issue 10, 1998, Pages 915-918

  Den Brok, S W J ^a  

^a JOHANNES GUTENBERG UNIVERSITY   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

CREEP; GRAIN BOUNDARIES; MICROCRACKING; MICROCRACKS; PRESSURE EFFECTS;

CRYSTALLOGRAPHIC ORIENTATIONS; DEFORMATION RATES; EFFECTIVE PRESSURE; EXPERIMENTAL EVIDENCE; GRAIN BOUNDARY STRUCTURE; MATERIAL TRANSPORT; ORDERS OF MAGNITUDE; THIN-FILM DIFFUSION;

STRAIN RATE;

CREEP; DEFORMATION MECHANISM; GRAIN BOUNDARY; MICROCRACK; PRESSURE SOLUTION; STRAIN;

EID: 84875001895     PISSN: 00917613     EISSN: None     Source Type: Journal    
DOI: 10.1130/0091-7613(1998)026<0915:EOMOPS>2.3.CO     Document Type: Article

References (3)

1. Atkinson, B. K., 1987, Fracture mechanics of rocks: London, Academic Press, 534 p.
2. Becker, A., 1995, Quartz pressure solution: Influence of crystallographic orientation: Journal of Structural Geology, v. 17, p. 1395-1405.
3. Bell, T. H., and Cuff, C., 1989, Dissolution, solution transfer, diffusion versus fluid flow and volume loss during deformation/metamorphism: Journal of Metamorphic Geology, v. 7, p. 425-447.