The Sinclair Caesium deposit occurs within a large differentiated pegmatite within the large pegmatite swarm adjacent to the Pioneer Dome. Several of these pegmatite intrusive bodies, including the PEG008 (or Sinclair Pegmatite) intrusive which hosts the Sinclair Caesium deposit, have a geochemical signature associated with the Lithium Caesium Tantalum (LCT) subclass of pegmatites (London 2008). The Peg008 pegmatite and Sinclair deposit are geologically similar to the large Tanco Mine at Bernic Lake, Manitoba.
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