Review paper
Magmatic systems of large continental igneous provinces
Volume: 8, Issue: 4, Pages: 621 - 640
Published: Jul 1, 2017
Abstract
Large igneous provinces (LIPs) formed by mantle superplume events have irreversibly changed their composition in the geological evolution of the Earth from high-Mg melts (during Archean and early Paleoproterozoic) to Phanerozoic-type geochemically enriched Fe-Ti basalts and picrites at 2.3 Ga. We propose that this upheaval could be related to the change in the source and nature of the mantle superplumes of different generations. The first...
Paper Details
Title
Magmatic systems of large continental igneous provinces
Published Date
Jul 1, 2017
Volume
8
Issue
4
Pages
621 - 640
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