Abstract
We present the first example of the phase transition occurring via the different kinetic mechanisms, displacive or diffusive, competing with each other in quartzlike single crystals. Upon room-pressure heating, transforms to the rutile-type phase (the transition) via the diffusive mechanism. With increase of the treatment pressure the diffusive mode of the temperature-induced transition is substituted at by a displacivelike mode, and then at the transition type changes from the sequence to a displacive martensiticlike transition to a distorted rutilelike phase (. A crossover between diffusive and displacive transition modes suggests a new way to control the meso- and nanometer-scale morphology of high-pressure phases.
- Received 15 August 2002
DOI:https://doi.org/10.1103/PhysRevLett.90.145503
©2003 American Physical Society