LONGITUDINAL PETROCHEMICAL VARIATION IN THE MACKENZIE DYKE SWARM, NORTHWESTERN CANADIAN SHIELD

Previous magnetic fabric studies of the giant, radiating, 1.27 Ga Mack enzie dyke swarm concluded that flow patterns within the dykes support the concept of a mantle plume that is centred beneath the swarm focus and supplies magma to overlying flood basalts and developing radial d ykes. To examine petrochemical implications of the model, compositiona l variation within the basalt sequence is compared with that of the dy kes along a 'stream line' of the swarm between 400 km (just beneath th e lavas) and 2100 km from its focus and in a parallel segment farther east. Evolution of tholeiitic magmas of the main sampled stream is rec orded in the upward change of composition in the lava sequence from mg -numbers of 70 to 35. Underlying (feeder) dykes have a comparable rang e, but outward along the swarm the range of compositions narrows progr essively towards its more evolved end, and at 2100 km, dyke compositio ns match those in upper levels of the lava sequence. REE and other tra ce element abundances show a similar contraction in range, and a shift towards more evolved compositions, both upward in the lava sequence a nd outward along the swarm. Apart from complications owing to crustal contamination, fundamental attributes of the magma (e.g Zr/Y) change l ittle with stratigraphic level or distance from the focus. The more ea sterly stream differs in its high proportion of alkalic compositions, suggesting the existence of distinctive subswarms. Normative mineral v ariation plots are consistent with fractionation in high- (main stream ) to low-level (eastern stream) crustal magma chambers. Mackenzie magm atism is compatible with the plume model. Domal uplift related to plum e activity initiated central graben collapse and outward-extending rad ial fractures, thus providing access to plume-derived magmas and loci for magma chamber and dyke swarm development. Multiple magma chambers, forming around the apex, each fed relatively independent subswarms of dykes. Uplift, accompanying fractionation, provided increasing magmat ic head by which fractionating magmas could be dispatched to successiv ely greater distances. This, and crystal settling in transport, accoun ts for the increasingly evolved nature of dykes with distance from the source.