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   <subfield code="a">The differentiation of the Skaergaard intrusion</subfield>
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   <subfield code="a">Conclusions: McBirney and Naslund have missed the two central points that we reiterate for clarity. First the composition of the cotectic cumulate extract for the LZc, best estimated from the average composition of adcumulate rocks, had a substantially lower silica content than any conceivable basaltic liquid, so silica enrichment is unavoidable. This is true of all the dyke compositions reported by Brooks and Nielsen, even the anomalous rock E with SiO2=46%. Second it is the normal behaviour of tholeiite basaltic magma to produce increasingly iron-rich cumulate extracts with little change in silica until FeTi oxide precipitation occurs when silica-enrichment and compositional divergence begins. Such divergence between equivalent cumulate plutonic and fractionated volcanic rocks hads been widely documented. Skaergaard magmas do have some uncommon features. However, similar assemblages exist in volcanic rocks as in the andesitic to rhyolitic glasses of the Loch Ba ring dyke, Mull (Sparks 1988). It is also a basic principle that elements enriched in cumulate rocks often become depleted in the corresponding liquids. Iron enrichment in the Skaergaard cumulates is complementary to iron depletion in liquids.</subfield>
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