Fluid participation in deep fault zones: Evidence from geological, geochemical, and <sup>18</sup>O/<sup>16</sup>O relationsR. Kerrich, Lisa Willmore, Timothy E. La Tour|Journal of Geophysical Research Atmospheres|1984Cited by 136
Mineral reactions participating in intragranular fracture propagation: implications for stress corrosion crackingR. Kerrich, Robert L. Barnett, Timothy E. La Tour|Journal of Structural Geology|1981Cited by 16
Chloritoid stability in very iron-rich altered pillow lavasTimothy E. La Tour, Robert L. Barnett, R. Kerrich et al.|Contributions to Mineralogy and Petrology|1980Cited by 8
Correction to “Fluid participation in deep fault zones: Evidence from geological, geochemical, and <sup>18</sup>O/<sup>16</sup>O relations” by R. Kerrich, T. E. La Tour, and L. WillmoreR. Kerrich, Lisa Willmore, Timothy E. La Tour|Journal of Geophysical Research Atmospheres|1985Cited by 0
138. Mineral Reactions Participating in Intragranular Fracture Propagation: Subcritical Crack Growth ?R. Kerrich, Robert L. Barnett, Timothy E. La Tour|Princeton University Press eBooks|1998Cited by 0