Depletion and refertilisation of the lithospheric mantle below the Kapsiki plateau (Northern Cameroon Volcanic Line) deduced from trace element and H2O systematics in mantle xenoliths

Author:

Nformidah-Ndah Siggy S.,Tollan Peter M.E.ORCID,Hermann Joerg,Tchouankoue Jean Pierre

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference139 articles.

1. Mineralogy and physico-chemical properties of Alluvial Clays from the Far-North region of Cameroon: a tool for an environmental problem;Adjia;Int. J. Water Resour. Environ. Eng.,2013

2. Characterization of spinel peridotites by olivine-spinel compositional relationships: review and interpretation;Arai;Chem. Geol.,1994

3. H2O Storage Capacity of Olivine at 5–8 GPa and Consequences for Dehydration Partial Melting of the Upper Mantle;Ardia,2012

4. High-pressure calibration of the olivineorthopyroxene-spinel oxygen barometer, implications for the oxidation state of the upper mantle;Ballhaus;Contrib. Mineral. Petrol.,1991

5. Depletion and enrichment processes in the lithospheric mantle beneath the Kola Peninsula (Russia): evidence from spinel lherzolite and wehrlite xenoliths;Beard;Lithos,2007

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