Metamorphic reaction rate controlled by fluid pressure not confining pressure: implications of dehydration experiments with gypsumSergio Llana‐Fúnez, D. R. Faulkner, John Wheeler|Contributions to Mineralogy and Petrology|2012Cited by 65
Electron Backscatter Diffraction (EBSD) Analysis of Bassanite Transformation Textures and Crystal Structure Produced from Experimentally Deformed and Dehydrated GypsumRebecca C. Hildyard, D. Prior, D. R. Faulkner et al.|Journal of Petrology|2011Cited by 41
Reaction fronts, permeability and fluid pressure development during dehydration reactionsHenri Leclère, John Wheeler, D. R. Faulkner et al.|Earth and Planetary Science Letters|2018Cited by 36
Fluid flow properties of Volterra Gypsum during experimental deformation at low strain rates monitored through simultaneous permeability measurementSergio Llana‐Fúnez, John Wheeler, D. R. Faulkner|EGU General Assembly Conference Abstracts|2009Cited by 1
Formation of secondary porosity in 4D Synchrotron X-ray tomography experimentsFlorian Fußeis, John Wheeler, Jie Liu et al.|EGU General Assembly Conference Abstracts|2010Cited by 0