Código QR (código de barras bidimensional)

Mantle Deformation Processes During the Rift‐To‐Drift Transition at Magma‐Poor Margins

Abstract The rift‐to‐drift transition at rifted margins is an area of active investigation due to an incomplete understanding of the spatial and temporal evolution of physical and chemical processes at the ocean‐continent transition (OCT). Deep structures that characterize modern OCTs are often diff...

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Bibliografiske detaljer
Principais autores: Nicholas J. Montiel, Emmanuel Masini, Luc Lavier, Othmar Müntener, Sylvain Calassou
Format: Artigo
Sprog:Inglês
Udgivet: Wiley 2023-11-01
Serier:Geochemistry, Geophysics, Geosystems
Fag:
Online adgang:https://doi.org/10.1029/2023GC010924
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