The quartz α↔β phase transition: Does it drive damage and reaction in continental crust?

@article{Johnson2021TheQ,
  title={The quartz $\alpha$↔$\beta$ phase transition: Does it drive damage and reaction in continental crust?},
  author={Scott E. Johnson and Won Joon Song and Alden C. Cook and Senthil S. Vel and Christopher C. Gerbi},
  journal={Earth and Planetary Science Letters},
  year={2021},
  volume={553},
  pages={116622}
}
2 Citations
Energy Partitioning, Dynamic Fragmentation, and Off‐Fault Damage in the Earthquake Source Volume
Seismological fracture or breakdown energy represents energy expended in a volume surrounding the advancing rupture front and the slipping fault surface. Estimates are commonly obtained by inverting

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The compressional and shear wave velocities in quarzite, granite, and granulite are determined at a fixed confining pressure of 2 kb as a function of temperature up to 720° C. The high-low quartz
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Rock rheology and density have first‐order effects on the lithosphere's response to plate tectonic forces at plate boundaries. Changes in these rock properties are controlled by metamorphic
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In the classical view of metamorphic microstructures, fast viscous relaxation (and so constant pressure) is assumed, with diffusion being the limiting factor in equilibration. This contribution is
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The thermally activated physical processes essential for earthquake source physics and the formation of mylonite layers and deep shear zones are examined. The possibility of the influence of
α/β phase transition in quartz monitored using acoustic emissions
SUMMARY It is usually suggested that thermal cracking in a quartz-bearing rock results from the anomalously high volumetric expansion coefficients of quartz (e.g. Simmons & Cooper 1978). It has also
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