Rejuvenated volcanism refers to the reemergence of volcanism after a hiatus of 0.5-2 Ma following the voluminous shield building stage of Hawaiian volcanoes. The composition of the rejuvenated source and its distribution relative to the center of the plu
Oceanic island basalts are targeted for geochemical study because they provide a direct window into ...
We present new isotopic and trace element data on post-shield alkalic lavas from the Hualalai, Mauna...
Numerous geochemical studies have indicated that the Hawaiian mantle plume consists of several disti...
International audienceThe “Koʻolau” component of the Hawaiian mantle plume represents an extreme (EM...
The alteration mineralogy, major and trace element chemistry, and Sr-Nd-Pb-Hf isotopic compositions ...
The South Kauaʻi Swell (SKS) volcano was sampled during four JASON dives and three dredge hauls reco...
Sr-Nd-Pb-Hf isotopic compositions of postshield lavas from two pairs of Hawaiian volcanoes, Mauna Ke...
We report and interpret new geochemical and Pb-Sr-Nd isotopic data from 325 samples of shield, late-...
Ocean island basalts are indirect records of Earth’s mantle chemistry and are fundamental for const...
Earth’s mantle is the most voluminous part of the planet and is inaccessible to direct investigation...
Oceanic island basalts provide the exceptional opportunity to study deep mantle geochemical reservoi...
There are geochemical differences between shield lavas from the two parallel trends, Kea and Loa, de...
We present new volatile, trace element, and radiogenic isotopic compositions for rejuvenated‐stage l...
[1] We report major and trace element and Sr and Nd isotope data for a 283 m thick sequence of posts...
International audienceThe radiogenic isotopic ratios of Sr, Nd, Hf, and Pb in basaltic lavas associa...
Oceanic island basalts are targeted for geochemical study because they provide a direct window into ...
We present new isotopic and trace element data on post-shield alkalic lavas from the Hualalai, Mauna...
Numerous geochemical studies have indicated that the Hawaiian mantle plume consists of several disti...
International audienceThe “Koʻolau” component of the Hawaiian mantle plume represents an extreme (EM...
The alteration mineralogy, major and trace element chemistry, and Sr-Nd-Pb-Hf isotopic compositions ...
The South Kauaʻi Swell (SKS) volcano was sampled during four JASON dives and three dredge hauls reco...
Sr-Nd-Pb-Hf isotopic compositions of postshield lavas from two pairs of Hawaiian volcanoes, Mauna Ke...
We report and interpret new geochemical and Pb-Sr-Nd isotopic data from 325 samples of shield, late-...
Ocean island basalts are indirect records of Earth’s mantle chemistry and are fundamental for const...
Earth’s mantle is the most voluminous part of the planet and is inaccessible to direct investigation...
Oceanic island basalts provide the exceptional opportunity to study deep mantle geochemical reservoi...
There are geochemical differences between shield lavas from the two parallel trends, Kea and Loa, de...
We present new volatile, trace element, and radiogenic isotopic compositions for rejuvenated‐stage l...
[1] We report major and trace element and Sr and Nd isotope data for a 283 m thick sequence of posts...
International audienceThe radiogenic isotopic ratios of Sr, Nd, Hf, and Pb in basaltic lavas associa...
Oceanic island basalts are targeted for geochemical study because they provide a direct window into ...
We present new isotopic and trace element data on post-shield alkalic lavas from the Hualalai, Mauna...
Numerous geochemical studies have indicated that the Hawaiian mantle plume consists of several disti...