New He, Nd, Pb, and Sr isotopic constraints on the constitution of the Hawaiian plume: Results from Koolau Volcano, Oahu, Hawaii, USA

Roden, Michael F.; Trull, Thomas W.; Hart, Stanley R.; Frey, Frederick A.

doi:10.1016/0016-7037(94)90547-9

Cited by 136 publications

(95 citation statements)

References 60 publications

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“…13); and (3) δ 18 O correlates with various radiogenic isotope ratios, although these correlations are dominated by differences between volcanoes rather than trends exhibited by lavas from any one volcano; see Eiler et al (1996b) for details of these correlations. Eiler et al (1996b) proposed that 18 Oenriched compositions in Koolau and Lanai lavas reflect a component of recycled uppercrustal rocks and/or sediments in their mantle sources, in agreement with previous suggestions that such components can explain 'enriched' trace-element and radiogenicisotope compositions of these lavas (Roden et al 1994). This interpretation has been followed by more recent papers adding Os isotope constraints (Hauri 1996;Lassiter and Hauri 1996), but argued against on the basis of some of the same data (Bennett et al 1996).…”

Section: Detailed Studiessupporting

confidence: 66%

Oxygen Isotope Variations of Basaltic Lavas and Upper Mantle Rocks

Eiler

2001

Reviews in Mineralogy and Geochemistry

639

374

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Section: Detailed Studiessupporting

confidence: 66%

Oxygen Isotope Variations of Basaltic Lavas and Upper Mantle Rocks

Eiler

2001

Reviews in Mineralogy and Geochemistry

639

374

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“…Haleakala (Kurz et al 1987), 25. Koolau (Roden et al 1994), 26. Kauai (Rison & Craig 1983, Mukhopadhyay et al 1996, 27.…”

Section: Heliumunclassified

Noble Gases in the Earth's Mantle

Farley

Neroda

1998

Annu. Rev. Earth Planet. Sci.

208

103

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Noble gas isotopic ratios in mantle-derived samples require variability in the timeintegrated ratio of volatile to lithophile elements in the Earth. Documentation of mantle 3 He/ 4 He variability is becoming increasingly complete, but for the heavier noble gases, the picture is still partly clouded by the effects of atmospheric contamination of mantle samples. Nevertheless, clear variations in mantle Ne, Ar, and Xe isotopic ratios exist, are apparently correlated with 3 He/ 4 He, and may be the product of varying degrees of mantle degassing. However, uncertainties in noble gas geochemical behavior and several conflicting observations leave open other possibilities. Recent Ne isotopic data are particularly important because they require that the atmosphere has not been closed to exchange with space. Derivation of much of the atmosphere from a source other than degassing of the mantle is a strong possibility that complicates efforts to model the geochemical evolution of the Earth.

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“…Multiple chemical components (HART et al, 1992;RODEN et al, 1994), radial (DEPAOLO et al, 2001) and asymmetric (ABOUCHAMI et al, 2005) zonation of the mantle plume source have been invoked to explain the chemical heterogeneity found in the volcanoes. The ability to characterize the temporal evolution of the volcanoes, and to tie the lava geochemistry to the structure of the mantle plume, is critically dependent on accurate dating of the lavas.…”

Section: Introductionmentioning

confidence: 99%