Mesoarchean melting and Neoarchean to Paleoproterozoic metasomatism during the formation of the cratonic mantle keel beneath West Greenland

Highly siderophile element (HSE) concentration and 187 Os/ 188 Os isotopic heterogeneity has been observed on various scales in the Earth's mantle. Interaction of residual mantle peridotite with infiltrating melts has been suggested to overprint primary bulk rock HSE signatures originating from...

Full description

Bibliographic Details
Published in:Geochimica et Cosmochimica Acta
Main Authors: van Acken, David, Luguet, Ambre, Pearson, D.G., Nowell, G.M., Fonseca, R.O.C., Nagel, Thorsten, Schulz, T.
Format: Article in Journal/Newspaper
Language:English
Published: 2017
Subjects:
Online Access:https://pure.au.dk/portal/da/publications/mesoarchean-melting-and-neoarchean-to-paleoproterozoic-metasomatism-during-the-formation-of-the-cratonic-mantle-keel-beneath-west-greenland(5fc192ce-50e7-48cb-9d10-b29083d722ba).html
https://doi.org/10.1016/j.gca.2017.01.006