Journal
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
Volume 6, Issue -, Pages -Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1029/2004GC000757
Keywords
Emperor Seamounts; Hawaiian hot spot; Hf isotopic ratio; mantle heterogeneity; geochemistry : radiogenic isotope geochemistry; geochemistry : composition of the mantle; geochemistry : major and trace element geochemistry; geodesy and gravity : earth's interior : composition and state; geographic location : pacific ocean
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The radiogenic isotopic ratios of Sr, Nd, Hf, and Pb in basaltic lavas associated with major hot spots, such as Hawaii, document the geochemical heterogeneity of their mantle source. What processes created such heterogeneity? For Hawaiian lavas there has been extensive discussion of geochemically enriched source components, but relatively little attention has been given to the origin of depleted source components, that is, components with the lowest Sr-87/Sr-86 and highest Nd-143/Nd-144 and Hf-176/Hf-177. The surprisingly important role of a depleted component in the source of the incompatible element-enriched, rejuvenated-stage Hawaiian lavas is well known. A depleted component also contributed significantly to the similar to76 - 81 Ma lavas erupted at Detroit Seamount in the Emperor Seamount Chain. In both cases, major involvement of MORB-related depleted asthenosphere or lithosphere has been proposed. Detroit Seamount and rejuvenated-stage lavas, however, have important isotopic differences from most Pacific MORB. Specifically, they define trends to relatively unradiogenic Pb isotope ratios, and most Emperor Seamount lavas define a steep trend of Hf-176/Hf-177 versus Nd-143/Nd-144. In addition, lavas from Detroit Seamount and recent rejuvenatedstage lavas have relatively high Ba/Th, a characteristic of lavas associated with the Hawaiian hot spot. It is possible that a depleted component, intrinsic to the hot spot, has contributed to these young and old lavas related to the Hawaiian hot spot. The persistence of such a component over 80 Myr is consistent with a long-lived source, i. e., a plume.
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