Coupled supercontinent–mantle plume events evidenced by oceanic plume record
Abstract
The most dominant features in the present-day lower mantle are the two antipodal African and Pacific large low-shear-velocity provinces (LLSVPs). How and when these two structures formed, and whether they are fixed and long lived through Earth history or dynamic and linked to the supercontinent cycles, remain first-order geodynamic questions. Hotspots and large igneous provinces (LIPs) are mostly generated above LLSVPs, and it is widely accepted...
Paper Details
Title
Coupled supercontinent–mantle plume events evidenced by oceanic plume record
Published Date
Nov 22, 2019
Journal
Volume
48
Issue
2
Pages
159 - 163
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Notes
History