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Considering the younger age recorded by both Re–Os and Pt–Os systems, we propose that the Pt–Os isochron age records a late, low temperature hydrothermal event affecting PGM and sulphides in the Platreef and Merensky Reef.
Pt-rich phases may also yield single grain Os can be well constrained.
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Nonetheless, the potential for the Pt–Os system in dating events in PGE mineralised systems is evident and the agreement of single grain model ages in high Pt/Os phases with the Pt–Os and Re–Os isochron ages indicates their usefulness in the geochronology of these systems.
Os isotope decay system can be measured by laser ablation MC-ICPMS.
► Pt-Os isochron for Merensky PGM is consistent with Re-Os ages.
► Pt-Os and Re-Os ages suggest that a late hydrothermal event may have occurred, affecting sulphides and PGM in the Merensky Reef and Platreef.
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