A heterogeneous subcontinental mantle under the African–Arabian Plate boundary revealed by boron and radiogenic isotopes

Abstract The northern and northwestern margins of the Arabian Plate are a locus of a diffuse and long-lasting (early Miocene to Pleistocene) Na-alkali basaltic volcanism, sourced in the asthenosphere mantle. The upwelling asthenosphere at the Africa–Arabia margin produces very limited magma volumes...

Disgrifiad llawn

Manylion Llyfryddiaeth
Prif Awduron: Samuele Agostini, Paolo Di Giuseppe, Piero Manetti, Carlo Doglioni, Sandro Conticelli
Fformat: Erthygl
Iaith:English
Cyhoeddwyd: Nature Portfolio 2021-05-01
Cyfres:Scientific Reports
Mynediad Ar-lein:https://doi.org/10.1038/s41598-021-90275-7