Mantle xenoliths from two larger Tertiary necks of Sal Island were studied in order to highlight the evolution of the Cape Verde (CV) lithospheric mantle. Xenoliths were are constituted by anhydrous spinel-bearing lherzolites, harbugites and minor wehrlites, with widespread metsomatic textures
|Number of pages||1|
|Journal||Geochimica et Cosmochimica Acta|
|Issue number||15, Supplement|
|Publication status||Published - Aug 2002|
Bonadiman, C., Beccaluva, L., Coltorti, M., & Siena, F. (2002). Garnet-spinel subsolidus reequilibration and K-metasomatism in Cape Verde lithospheric mantle. Geochimica et Cosmochimica Acta, 66(15, Supplement), 90-90.