Computer Science
Scientific paper
Oct 1986
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1986e%26psl..80...55t&link_type=abstract
Earth and Planetary Science Letters, Volume 80, Issue 1-2, p. 55-70.
Computer Science
1
Scientific paper
Recent Nd-Sr-Pb isotope studies of Caledonian granitoids [1-4] have reopened the question of the existence of an unusual or enriched mantle source beneath Caledonian Scotland. This was postulated [5] following a Nd-Sr isotope geochemical study of lavas associated with the Scottish Old Red Sandstone. Pb isotope data for the same lavas reported here restrict any major crustal involvement in southwest Highland primitive lavas to ca. 1750 Ma old Rb-depleted granulites. The lack of such crustal material within Scotland together with Pb-Sr isotopic relationships strongly suggests that a large volume mantle source with low μ, Rb/Sr and Sm/Nd has been present at depth under western Scotland since the early Proterozoic. It is unlikely that this is the same enriched mantle source observed from xenoliths in younger magmas [25], and is probably located deep in the lithosphere or within the asthenosphere. This source has contributed extensively to the incompatible element budget of Caledonian granitoids implying that the Caledonian orogeny did result in significant growth of the British crust.
Present address: Department of Geology, RHB New College, Egham Hill, Egham, Surrey, U.K.
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