Tracing the HIMU component within Pan-African lithosphere beneath northeast Africa: Evidence from Late Cretaceous Natash alkaline volcanics, Egypt-Reference-Cited by-同舟云学术

Tracing the HIMU component within Pan-African lithosphere beneath northeast Africa: Evidence from Late Cretaceous Natash alkaline volcanics, Egypt

Published:2018-02 Issue: Volume:300-301 Page:136-153
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Abu El-Rus M.A.,Chazot G.,Vannucci R.,Paquette J.-L.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

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1. Mineralogical and geochemical characterization of the Wadi Natash volcanic field (WNVF), Egypt: Alkaline magmatism in a Late Cretaceous continental rift system;Acta Geochimica;2024-06-27

2. Origin and evolution of lithospheric mantle beneath the juvenile Arabian–Nubian Shield: Evidence from the Natash peridotite xenoliths, Southern Eastern Desert, Egypt;Lithos;2024-03

3. Petrogenesis of Late Cretaceous A1-type alkali monogenetic volcanoes, Wadi Natash, South Eastern Desert, Egypt, and their implications for Nb mineralization and tectonic evolution;Arabian Journal of Geosciences;2023-08-29

4. A case of Ampferer-type subduction beneath the New Caledonia arc: Evidence for inefficient subduction of hydrated lithologies into the upper mantle;GSA Bulletin;2022-08-26

5. Hidden but Ubiquitous: The Pre-Rift Continental Mantle in the Red Sea Region;Frontiers in Earth Science;2021-08-02