HAL (France)open access
Sub-continental lithospheric mantle beneath the Adamawa volcanic area (Cameroon Volcanic Line): inference from lavas and hosted mantle xenoliths from Bini Warack, NE-Ngaoundéré, Cameroon (Central Africa)
Low partial melting degrees, Cameroon Volcanic Line, 1, Mantle xenoliths, Carbonate metasomatism, 2, 0, OIB affinity
This document is indexed with metadata only — full text is not available in the archive for this record.
Open the official source ↗
Record · ID 202502
Retrieved via
Conceptio — every document is proof-bundled with source, license, and retrieval metadata.