EGU22-11558
https://doi.org/10.5194/egusphere-egu22-11558
EGU General Assembly 2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Nanoscale apatite inclusions in xenotime: witness of Pb mobility

Cilva Joseph
Cilva Joseph
  • Curtin University, Earth and Planetary Sciences, Australia (cilva.joseph@postgrad.curtin.edu.au)

Nanoscale apatite inclusions in xenotime: witness of Pb mobility

Cilva Joseph1, 2, Denis Fougerouse1, 2, Steven M. Reddy1, 2, Aaron Dodd3, Steven Denyszyn4, David W. Saxey2, William D.A. Rickard2

1School of Earth and Planetary Sciences, Curtin University, Perth, Australia

2Geoscience Atom Probe Facility, John de Laeter Centre, Curtin University, Perth, Australia

3Microscopy and Microanalysis Facility, John De Laeter Centre, Curtin University, Perth, Australia

4School of Earth Sciences, University of Western Australia, Perth, Australia

Discordant ages as measured by 206Pb/238U and 207Pb/235U ratios in various geochronometers are common. Several mechanisms have been proposed to explain discordant ages in different minerals. These include loss of radiogenic Pb, mixing of different age domains within a mineral, and intermediate daughter radioisotope disequilibrium. Xenotime (YPO4) is a geochronometer used to date different geological processes, such as diagenesis, metamorphism, and hydrothermal events. However, xenotime commonly yields small degrees of discordancy (<3%) by high precision geochronology techniques. To investigate the mechanism responsible for slightly discordant xenotime analyses, two ~1000 Ma crystals (z6413 and Y1) from Ontario and Western Australia were analysed using atom probe tomography (APT) and transmission electron microscopy (TEM) which provide sub-nanometre scale chemical and crystallographic analysis of minerals. Both samples have not undergone significant metamorphism (T < 300°C) after crystallisation. Combined APT and TEM results revealed the presence of nanoscale apatite [Ca5(PO4)3(F,Cl,OH)] inclusions and crystal dislocations in the xenotime grains. APT data indicates that the apatite inclusions are rich in radiogenic Pb and that the dislocations are decorated with Ca, Cl and H. Nanogeochronology of xenotime by APT indicate that the apatite inclusions likely formed by exsolution during the cooling of crystals, capturing radiogenic Pb. Dislocations in the crystals may have acted as fast diffusion pathways leading to radiogenic Pb-loss and caused the U-Pb system disturbance.

How to cite: Joseph, C.: Nanoscale apatite inclusions in xenotime: witness of Pb mobility, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-11558, https://doi.org/10.5194/egusphere-egu22-11558, 2022.

Comments on the display material

to access the discussion