Abstract
The results of a magnetometric survey of the Alnö Complex suggest that it consists of the main intrusion in the north-eastern part of Alnö Island, a satellite intrusion of mainly carbonatite at Söråker (measuring about 1 × 1.4 km) and the earlier recognized satellite vent at Båräng. The new picture of the Alnö Complex, which is in striking contrast to the views of von Eckermann, is discussed.

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