A Highly Depleted and Subduction‐Modified Mantle Beneath the Slow‐Spreading Mohns Ridge

Abstract The Mohns Ridge is a very slow‐spreading ridge that, together with the Knipovich Ridge, marks the boundary between the North American and Eurasian plates in the Norwegian‐Greenland Sea. In this study, we report the major and trace element composition of spatially associated basalts and peri...

ver descrição completa

Detalhes bibliográficos

Principais autores:	A. Bjerga, H. H. Stubseid, L. E. R. Pedersen, A. Beinlich, R. B. Pedersen
Formato:	Artigo
Idioma:	Inglês
Publicado em:	Wiley 2022-11-01
coleção:	Geochemistry, Geophysics, Geosystems
Assuntos:	abyssal peridotite tectonic window Arctic Ocean chromium spinel partial melting melt‐rock interaction
Acesso em linha:	https://doi.org/10.1029/2022GC010585
Tags:	Adicionar Tag Sem tags, seja o primeiro a adicionar uma tag!