The Putorana basalts, comprising similar to 90% of the Siberian Traps
(ST), have had their chemistry modified from primary tholeiitic picrit
ic magmas by similar to 12% crystallization of olivine. Major-trace el
ement ratios, and Nd isotopes of these lavas are consistent with their
origin from a relatively undepleted plume by 12-16% rapid decompressi
onal melting at similar to 50-80 km depths within the lithosphere.