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.
Michaela Flanigan
Researcher
Michaela Flanigan uses radiogenic isotope systems to investigate the geochemical origins of oceanic volcanism in the southwest Pacific.