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• Zircon/fluid trace element partition coefficients measured by recrystallization of Mud Tank zircon at 1.5 GPa and 800–1000 °C - ScienceDirect

Zircon/fluid trace element partition coefficients measured by recrystallization of Mud Tank zircon at 1.5 GPa and 800–1000 °C - ScienceDirect

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Zircon Hf isotope behavior during the magmatic-hydrothermal processes: A case study from the Yashan pluton, South China - ScienceDirect

The influence of microscale lithological layering and fluid availability on the metamorphic development of garnet and zircon: insights into dissolution–reprecipitation processes, Mineralogical Magazine

SIMS determination of trace element partition coefficients between garnet, clinopyroxene and hydrous basaltic liquids at 2–7.5 GPa and 1080–1200°C - ScienceDirect

Partition coefficients of REEs in apatite/melt and zircon/melt

PDF) Decoupling of zircon U–Pb and trace-element systematics

PDF) Re-equilibration of Zircon in Aqueous Fluids and Melts

Zircon Hf isotope behavior during the magmatic-hydrothermal processes: A case study from the Yashan pluton, South China - ScienceDirect

Zircon/fluid trace element partition coefficients measured by recrystallization of Mud Tank zircon at 1.5 GPa and 800–1000 °C - ScienceDirect

Trace elements partition coefficient between zircon and coexisting

Experimental zircon/melt and zircon/garnet trace element partitioning and implications for the geochronology of crustal rocks - ScienceDirect

The influence of microscale lithological layering and fluid availability on the metamorphic development of garnet and zircon: insights into dissolution–reprecipitation processes, Mineralogical Magazine

Zircon/fluid trace element partition coefficients measured by recrystallization of Mud Tank zircon at 1.5 GPa and 800–1000 °C - ScienceDirect