The hydrothermal stability of zircon - Preliminary experimental and isotopic studies

Details The hydrothermal stability of zircon - Preliminary experimental and isotopic studies The hydrothermal stability of zircon - Preliminary experimental and isotopic studies

Sep 1992

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992gecoa..56.3551k&link_type=abstract

Geochimica et Cosmochimica Acta (ISSN 0016-7037), vol. 56, no. 9, Sept. 1992, p. 3551-3660.

Other

11

Crystal Defects, Geochemistry, Geochronology, Hydrothermal Systems, Scanning Electron Microscopy, Annealing, Earth Crust, Lead Isotopes, Silicon Oxides, Uranium Isotopes, Zirconium Oxides

Scientific paper

U-Pb isotopic discordance in experimentally treated zircons is characterized as a function of the solution composition, P-T conditions, and time. Backscattered electron imaging of the run products suggests that partial homogenization of chemical zoning patterns occurred during the experiments. Microprobe analyses of treated and untreated grains show that both populations have a similar range of Hf contents.

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