The xenoliths from the Senegal Cape Verde Peninsula originate from a Rare Earth-depleted spinel lherzolite mantle source zone. The low contents of incompatible elements (Ce, La), high Ni and Cr ...
The enrichment in LREE relative to the HREE of the dolerites studied associated with the ratios (Tb/Yb)N (1.95 - 2.56), Dy/Yb (2.33 - 2.85) characterizes a mantle source of lherzolite with garnet.
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