Abstract
There is a progressive secular decline in light-RE enrichment from Tertiary to Present, similar to that previously observed on the Faeroes 50–60mybp. Light-RE depleted oceanic type patterns appear on Iceland only within the last 0.7my. These results suggest pulsating mantle plume activity with time and provide further support to the blob model previously proposed for the origin of the Faeroes-Iceland-Greenland Ridge. Available Sr and Nd isotopic data are consistent with the model.
Regular spatial variations are observed within the SW and SE neovolcanic zones. (La/Sm) decreases and Mg-values increase toward Central Iceland in both zones but at a faster rate in the SE zone. These spatial variations and available isotopic and heat flow data are best explained by a temporal change in melting conditions due to southward propagations of rifts from Central Iceland, starting approximately 6mybp along the SW zone and more recently along the SE zone. The SW zone has now reached thermal maturity, and basalts derived from the upper mantle are composed of a mix of light-RE enriched plume material and depleted asthenospheric material. The SE zone is still in a transient stage of evolution, and lavas from the tip of the propagating rift are derived by melting of the older Late-Miocene lower crust-lithosphere, whereas in the northern part of the zone, lavas are derived from a mantle plume-asthenospheric mix now dominated by the latter type of material. In contrast, there is no geochemical evidence of rift propagation in northern Iceland, as no systematic variations have been observed along either the NE neovolcanic zone or the Skagi paleorift zone.
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Schilling, JG., Meyer, P.S., Kingsley, R.H. (1983). Rare Earth Geochemistry of Iceland Basalts: Spatial and Temporal Variations. In: Bott, M.H.P., Saxov, S., Talwani, M., Thiede, J. (eds) Structure and Development of the Greenland-Scotland Ridge. Nato Conference Series, vol 8. Springer, Boston, MA. https://doi.org/10.1007/978-1-4613-3485-9_17
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