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
Crustal outgassing and LILE enrichment in major lithosphere structures, Archean Abitibi greenstone belt: evidence on the source reservoir from strontium and carbon isotope tracersR. Kerrich, E. van Hees, Brian J. Fryer et al.|Contributions to Mineralogy and Petrology|1987Cited by 69
Corundum, Cr-muscovite rocks at O'Briens, Zimbabwe: the conjunction of hydrothermal desilicification and LIL-element enrichment ? geochemical and isotopic evidenceR. Kerrich, Lisa Willmore, W. S. Fyfe et al.|Contributions to Mineralogy and Petrology|1987Cited by 36
Reply to: ?A discussion of corundum, Cr-muscovite rocks at O'Briens, Zimbabwe: the conjunction of hydrothermal desilicification and LIL-element enrichment-geochemical and isotopic evidence/rdR. Kerrich, Lisa Willmore, W. S. Fyfe et al.|Contributions to Mineralogy and Petrology|1988Cited by 4
Source terranes, magmatic evolution, and hydrothermal regimes in the Mo-, Sn-mineralized Ackley Granite, Newfoundland; evidence from combined geochemical and oxygen isotope dataJ. Tuach, F Strong David, R. Kerrich et al.|Unknown|1988Cited by 2