Abstract
With mantle xenoliths from Tallante (South Spain) incompatible elements and Sr-Nd isotopes record in most samples widespread enrichments produced by percolation of Na-alkaline melts (by both porous flow and open-conduit mechanisms) leading to variably vein xenoliths. On the other hand, 3 samples out of 55, containing traces of amphibole and phlogopite and characterised by relatively high SiO2 content (and high modal abundance of opx) display enrichments characterised by a completely different geochemical fingerprint.
Original language | English |
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Pages (from-to) | 59-59 |
Number of pages | 1 |
Journal | Geochimica et Cosmochimica Acta |
Volume | 66 |
Issue number | 15, Supplement |
Publication status | Published - Aug 2002 |
Externally published | Yes |