Deformation mechanisms and rheology: why marble is weaker than quartzite
Author:
Publisher
Geological Society of London
Subject
Geology
Reference23 articles.
1. Diffusion-accommodated flow and superplasticity
2. Thermally-induced grain growth of calcite marbles on Naxos Island, Greece
3. Quartz deformation in a very fine grained quartzo-feldspathic mylonite: a lack of evidence for dominant grain boundary sliding deformation
4. A flow law for dislocation creep of quartz aggregates determined with the molten salt cell
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