Abstract
Ion microprobe U-Pa measurements in zircon crystals from a Holocene rhyolite (Salton Buttes, California) are utilized to assess the partitioning of Pa and U between zircon and melt. The relative sensitivity factor (RSF) for ion microprobe U-Pa zircon analysis was calibrated on a natural high-U secular equilibrium zircon from Buff Peak (Nevada). Zircon crystals from Salton Buttes rhyolite show evidence for excess 231Pa with a weighted average (231Pa)/(235U) activity ratio of 1.9. From this ratio, model zircon-melt partition coefficient ratios DPa/DU = 0.9.2.2 are obtained, assuming plausible limits for (231Pa)/(235U)melt and correcting for the age of zircon crystallization (~15 ka). These values roughly fit lattice strain models for tetravalent cations, but are more than one order of magnitude lower than predictions for pentavalent Pa. Based on this appraisal of Pa partitioning, initial 231Pa disequilibrium caused by zircon-melt fractionation alone can produce minor discordance or excess 207Pb in Late Cenozoic zircon, but is insignificant for older U-Pb zircon ages.
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
- New constraints on metamorphic history of Adirondack diopsides (New York, U.S.A.): Al and δ18O profiles
- Hammadah al Hamra 193: The first amphibole-bearing winonaite
- Crystal chemistry of trioctahedral micas in alkaline and subalkaline volcanic rocks: A case study from Mt. Sassetto (Tolfa district, Latium, central Italy)
- Magnetic excitations and heat capacity of fayalite, Fe2SiO4
- The barometer tremolite + tschermakite + 2 albite = 2 pargasite + 8 quartz: Constraints from experimental data at unit silica activity, with application to garnet-free natural assemblages
- In-situ measurement of dissolution of anorthite in Na-Cl-OH solutions at 22 °C using phase-shift interferometry
- Experimental investigation of the breakdown of dolomite in rock cores at 100 MPa, 650-750 °C
- Dissolution of the (001) surface of galena: An in situ assessment of surface speciation by fluid-cell micro-Raman spectroscopy
- An infrared spectroscopic study of the OH stretching frequencies of talc and 10-Å phase to 10 GPa
- Co2+-Cu2+ substitution in bieberite solid-solution series, (Co1-xCux)SO4·7H2O, 0.00 ≤ x ≤ 0.46: Synthesis, single-crystal structure analysis, and optical spectroscopy
- Clinoenstatite exsolution in diopsidic augite of Dabieshan: Garnet peridotite from depth of 300 km
- Heat-pulse calorimetry measurements on natural chlorite-group minerals
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- Single-crystal elasticity of zoisite Ca2Al3Si3O12(OH) by Brillouin scattering
- The effect of valence state and site geometry on Ti L3,2 and O K electron energy-loss spectra of TixOy phases
- Characterization of defects and the local structure in natural and synthetic alunite (K, Na, H3O)Al3(SO4)2(OH)6 by multi-nuclear solid-state NMR spectroscopy
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- Transmission electron microscopy study of magnetites in a freshwater population of magnetotactic bacteria
- Anomalous behavior at the I2/a to Imab phase transition in SiO2-moganite: An analysis using hard-mode Raman spectroscopy
- The system Ag-Au-Se: Phase relations below 405 K and determination of standard thermodynamic properties of selenides by solid-state galvanic cell technique
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