Variable helium diffusion characteristics in fluorite

• Published in: Geochimica et cosmochimica acta Vol. 188; pp. 21 - 34
• Main Authors: Wolff, R., Dunkl, I., Kempe, U., Stockli, D., Wiedenbeck, M., von Eynatten, H.
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01.09.2016
• Subjects: Diffusion; Fluorite; Helium; Thermochronology; Fluorite; Helium; Diffusion; Thermochronology
• ISSN: 0016-7037; 1872-9533
• DOI: 10.1016/j.gca.2016.05.029

Precise analysis of the diffusion characteristics of helium in fluorite is crucial for establishing the new fluorite (U–Th–Sm)/He thermochronometer (FHe), which potentially provides a powerful tool for dating ore deposits unsuitable for the application of conventional geochronometers. Incremental helium outgassing experiments performed on fluorites derived from a spectrum of geological environments suggest a thermally activated volume diffusion mechanism. The diffusion behaviour is highly variable and the parameters range between logD0/a2=0.30±0.27–7.27±0.46s−1 and Ea=96±3.5–182±3.8kJ/mol. Despite the fact that the CaF2 content of natural fluorites in most cases exceeds 99 weight percent, the closure temperature (Tc) of the fluorite (U–Th–Sm)/He thermochronometer as calculated from these diffusion parameters varies between 46±14°C and 169±9°C, considering a 125μm fragment size. Here we establish that minor substitutions of calcium by rare earth elements and yttrium (REE+Y) and related charge compensation by sodium, fluorine, oxygen and/or vacancies in the fluorite crystal lattice have a significant impact on the diffusivity of helium in the mineral. With increasing REE+Y concentrations F vacancies are reduced and key diffusion pathways are narrowed. Consequently, a higher closure temperature is to be expected. An empirical case study confirms this variability: two fluorite samples from the same deposit (Horni Krupka, Czech Republic) with ca. 170°C and ca. 43°C Tc yield highly different (U–Th–Sm)/He ages of 290±10Ma and 79±10Ma, respectively. Accordingly, the fluorite sample with the high Tc could have quantitatively retained helium since the formation of the fluorite-bearing ores in the Permian, despite subsequent Mesozoic burial and associated regional hydrothermal heating. In contrast, the fluorite with the low Tc yields a Late Cretaceous age close to the apatite fission track (AFT) and apatite (U–Th)/He ages (AHe) from the same locality. Remarkably, thermal modelling of FHe yields comparable results to the well-established modelling based on AFT and AHe.