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dc.contributor.authorPhillips, Erin H.  Concept link
dc.contributor.authorSims, Kenneth W. W.  Concept link
dc.contributor.authorSherrod, David R.  Concept link
dc.contributor.authorSalters, Vincent J. M.  Concept link
dc.contributor.authorBlusztajn, Jerzy S.  Concept link
dc.contributor.authorDulai, Henrietta  Concept link
dc.date.accessioned2017-02-10T18:51:00Z
dc.date.available2018-08-20T08:36:46Z
dc.date.issued2016-08
dc.identifier.urihttps://hdl.handle.net/1912/8691
dc.description© The Author(s), 2016. This is the author's version of the work and is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Geochimica et Cosmochimica Acta 195 (2016): 201-225, doi:10.1016/j.gca.2016.08.017.en_US
dc.description.abstractTo understand the dynamics of solid mantle upwelling and melting in the Hawaiian plume, we present new major and trace element data, Nd, Sr, Hf, and Pb isotopic compositions, and 238U-230Th-226Ra and 235U-231Pa-227Ac activities for 13 Haleakala Crater nepheline normative basanites with ages ranging from ~900 to 4100 yr B.P.. These basanites of the Hana Volcanics exhibit an enrichment in incompatible trace elements and a more depleted isotopic signature than similarly aged Hawaiian shield lavas from Kilauea and Mauna Loa. Here we posit that as the Pacific lithosphere beneath the active shield volcanoes moves away from the center of the Hawaiian plume, increased incorporation of an intrinsic depleted component with relatively low 206Pb/204Pb produces the source of the basanites of the Hana Volcanics. Haleakala Crater basanites have average (230Th/238U) of 1.23 (n=13), average age-corrected (226Ra/230Th) of 1.25 (n=13), and average (231Pa/235U) of 1.67 (n=4), significantly higher than Kilauea and Mauna Loa tholeiites. U-series modeling shows that solid mantle upwelling velocity for Haleakala Crater basanites ranges from ~0.7 to 1.0 cm/yr, compared to ~10 to 20 cm/yr for tholeiites and ~1 to 2 cm/yr for alkali basalts. These modeling results indicate that solid mantle upwelling rates and porosity of the melting zone are lower for Hana Volcanics basanites than for shield-stage tholeiites from Kilauea and Mauna Loa and alkali basalts from Hualalai. The melting rate, which is directly proportional to both the solid mantle upwelling rate and the degree of melting, is therefore greatest in the center of the Hawaiian plume and lower on its periphery. Our results indicate that solid mantle upwelling velocity is at least 10 times higher at the center of the plume than at its periphery under Haleakala.en_US
dc.description.sponsorshipFunding for this project was provided by NSF grants EAR-0001924 and EAR-9909473 to KWWS.en_US
dc.language.isoen_USen_US
dc.relation.urihttps://doi.org/10.1016/j.gca.2016.08.017
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 International*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.titleIsotopic constraints on the genesis and evolution of basanitic lavas at Haleakala, Island of Maui, Hawaiien_US
dc.typePreprinten_US
dc.description.embargo2018-08-20en_US


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Attribution-NonCommercial-NoDerivatives 4.0 International
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivatives 4.0 International