A mantle plume origin for the Palaeoproterozoic Circum-Superior Large Igneous Province
Abstract
The Circum-Superior Large Igneous Province (LIP) consists predominantly of ultramafic-mafic lavas and sills with minor felsic components, distributed as various segments along the margins of the Superior Province craton. Ultramafic-mafic dykes and carbonatite complexes of the LIP also intrude the more central parts of the craton. Most of this magmatism occurred ∼1880 Ma. Previously a wide range of models have been proposed for the different...
Paper Details
Title
A mantle plume origin for the Palaeoproterozoic Circum-Superior Large Igneous Province
Published Date
Jun 1, 2017
Journal
Volume
294
Pages
189 - 213
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