A Caltech Library Service

Are high ^3He/^4He ratios in oceanic basalts an indicator of deep-mantle plume components?

Meibom, Anders and Anderson, Don L. and Sleep, Norman H. and Frei, Robert and Chamberlain, C. Page and Hren, Michael T. and Wooden, Joseph L. (2003) Are high ^3He/^4He ratios in oceanic basalts an indicator of deep-mantle plume components? Earth and Planetary Science Letters, 208 (3-4). pp. 197-204. ISSN 0012-821X. doi:10.1016/S0012-821X(03)00038-4.

Full text is not posted in this repository. Consult Related URLs below.

Use this Persistent URL to link to this item:


The existence of a primordial, undegassed lower mantle reservoir characterized by high concentration of ^3He and high ^3He/^4He ratios is a cornerstone assumption in modern geochemistry. It has become standard practice to interpret high ^3He/^4He ratios in oceanic basalts as a signature of deep-rooted plumes. The unfiltered He isotope data set for oceanic spreading centers displays a wide, nearly Gaussian, distribution qualitatively similar to the Os isotope (^(187)Os/^(188)Os) distribution of mantle-derived Os-rich alloys. We propose that both distributions are produced by shallow mantle processes involving mixing between different proportions of recycled, variably aged radiogenic and unradiogenic domains under varying degrees of partial melting. In the case of the Re–Os isotopic system, radiogenic mid-ocean ridge basalt (MORB)-rich and unradiogenic (depleted mantle residue) endmembers are constantly produced during partial melting events. In the case of the (U+Th)–He isotope system, effective capture of He-rich bubbles during growth of phenocryst olivine in crystallizing magma chambers provides one mechanism for ‘freezing in’ unradiogenic (i.e. high ^3He/^4He) He isotope ratios, while the higher than chondritic (U+Th)/He elemental ratio in the evolving and partially degassed MORB melt provides the radiogenic (i.e. low ^3He/^4He) endmember. If this scenario is correct, the use of He isotopic signatures as a fingerprint of plume components in oceanic basalts is not justified.

Item Type:Article
Related URLs:
URLURL TypeDescription
Additional Information:© 2003 Elsevier Science B.V. Received 16 August 2002; received in revised form 13 November 2002; accepted 15 January 2003.
Subject Keywords:He isotopes; Os isotopes; plumes; upper mantle; lower mantle
Issue or Number:3-4
Record Number:CaltechAUTHORS:20121010-074950586
Persistent URL:
Official Citation:Anders Meibom, Don L. Anderson, Norman H. Sleep, Robert Frei, C.Page Chamberlain, Michael T. Hren, Joseph L. Wooden, Are high 3He/4He ratios in oceanic basalts an indicator of deep-mantle plume components?, Earth and Planetary Science Letters, Volume 208, Issues 3–4, 30 March 2003, Pages 197-204, ISSN 0012-821X, 10.1016/S0012-821X(03)00038-4. (
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:34805
Deposited By: Ruth Sustaita
Deposited On:10 Oct 2012 15:50
Last Modified:09 Nov 2021 23:10

Repository Staff Only: item control page