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1 Department of Geology, University of Leicester, Leicester LE1 7RH, England
Large igneous provinces, representing prodigious volumes of basalt erupted through continental and oceanic crust, are believed to be associated with high-temperature mantle plumes incident at the base of the lithosphere. Recent "plume initiation" models for continental flood-basalt volcanism suggest that material in the plume will intersect the solidus shortly after arriving, or impacting, beneath the lithosphere, so that melting is near-synchronous with plume impact. Beneath continents, however, melting of a plume head is inhibited by the presence of a thick (>125 km) mechanical boundary layer, which must be thinned and removed by conductive heating and melt injection before significant basalt production can occur. This necessitates a period of plume incubation, characterized by lithosphere extension and doming, by the establishment of long- lived paleodrainage patterns, and, laterally, by the intrusion of alkalic magmas. Field evidence from rive major igneous provinces indicates that plume incubation is a more appropriate model than simple plume impact for continental flood-basalt volcanism.
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