Thermochemical anomalies in the upper mantle control Gakkel Ridge accretion

The ultimate driver of ultraslow spreading ridges is unknown. Here the authors use spreading rates derived directly from isotopic ages of seafloor samples to link magmatic and amagmatic segments with thermochemical variations in the upper mantle.

Enregistré dans:
Détails bibliographiques
Auteurs principaux: John M. O’Connor, Wilfried Jokat, Peter J. Michael, Mechita C. Schmidt-Aursch, Daniel P. Miggins, Anthony A. P. Koppers
Format: article
Langue:EN
Publié: Nature Portfolio 2021
Sujets:
Q
Accès en ligne:https://doaj.org/article/dab11e69016a4d15a7e0b7e1061e70f6
Tags: Ajouter un tag
Pas de tags, Soyez le premier à ajouter un tag!