Global geochemical fingerprinting of plume intensity suggests coupling with the supercontinent cycle

Plate tectonics and mantle plumes are two of the most fundamental solid-Earth processes that have operated through much of Earth history. For the past 300 million years, mantle plumes are known to derive mostly from two large low shear velocity provinces (LLSVPs) above the core-mantle boundary, refe...

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Bibliographic Details
Main Authors: Gamal EL Dien, Hamed, Doucet, Luc, Li, Zheng-Xiang, Cox, Grant, Mitchell, Ross
Format: Journal Article
Language:English
Published: NATURE PUBLISHING GROUP 2019
Subjects:
Online Access:http://purl.org/au-research/grants/arc/FL150100133
http://hdl.handle.net/20.500.11937/90598