The isotopic origin of Lord Howe Island reveals secondary mantle plume twinning in the Tasman Sea
First radiogenic isotope data from Lord Howe Island lavas reveal a secondary mantle plume twin in the Tasman Sea with a distinct deep mantle source.
Ian Smith
Emeritus Associate Professor
Ian Smith uses geochemistry to understand volcanic systems, with a focus on the Auckland Volcanic Field and Late Cenozoic basaltic volcanism in the southwest Pacific.