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.
Mark Kendrick
Associate Professor of Geochemistry
Mark Kendrick uses noble gas isotopes and halogens to investigate the role of fluids and volatiles in geological processes from the Earth’s surface to the deep mantle, with interests in hydrothermal alteration and subduction zone processes.
Iron isotope systematics during igneous differentiation in lavas from Kīlauea and Mauna Loa, Hawai'i
Iron isotope and hafnium data from Kīlauea and Mauna Loa lavas reveal how igneous differentiation and mantle source heterogeneity shape Hawaiian volcanism.
