Lead Isotope Materials
Lead is one of the most frequently studied isotope systems in geochemistry. Based on geochemical findings and archaeological applications, lead-isotope signatures have, for instance, been used to trace the origin of archaeological artefacts.
|ERM-3800||solution||0 ‰ *|
|NRC SRM 981||elemental Pb||0 ‰|
* Exact value defining the δ208/206PbSRM981 scale.
The values listed in this table are compilation and are not necessarily CIAAW recommendations.