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Erik H. Hauri

Researcher at Carnegie Institution for Science

Publications -  249
Citations -  20515

Erik H. Hauri is an academic researcher from Carnegie Institution for Science. The author has contributed to research in topics: Mantle (geology) & Melt inclusions. The author has an hindex of 73, co-authored 245 publications receiving 18178 citations. Previous affiliations of Erik H. Hauri include University of Arizona & Woods Hole Oceanographic Institution.

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Mantle Plumes and Entrainment: Isotopic Evidence

TL;DR: Many oceanic island basalts show sublinear subparallel arrays in Sr-Nd-Pb isotopic space, but the depleted upper mantle is rarely a mixing end-member of these arrays, as would be expected if mantle plumes originated at a 670-kilometer boundary layer and entrained upper mantle during ascent.
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MPI-DING reference glasses for in situ microanalysis: New reference values for element concentrations and isotope ratios

Klaus Peter Jochum, +60 more
TL;DR: In this paper, the authors present new analytical data of major and trace elements for the geological MPI-DING glasses KL2-G, ML3B-G and ATHO-G.
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Vapour undersaturation in primitive mid-ocean-ridge basalt and the volatile content of Earth's upper mantle

TL;DR: The undersaturated pre-eruptive volatile content for a suite of mid-ocean-ridge basalts from the Siqueiros intra-transform spreading centre is reported, leading to correlations between volatiles and refractory trace elements that provide new constraints on volatile abundances and their behaviour in the upper mantle.
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Experimental and natural partitioning of Th, U, Pb and other trace elements between garnet, clinopyroxene and basaltic melts

TL;DR: Partition coefficients for Th, U, Pb, rare earth elements (REE), high field strength elements (HFSE), alkaline-earth elements, Sc, Cr, V and K were measured by ion microprobe techniques in two experiments on a natural high-alumina basalt composition from Medicine Lake, California as discussed by the authors.
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Volatile content of lunar volcanic glasses and the presence of water in the Moon’s interior

TL;DR: The results indicate that, contrary to prevailing ideas, the bulk Moon might not be entirely depleted in highly volatile elements, including water, and the presence of water must be considered in models constraining the Moon’s formation and its thermal and chemical evolution.