[1]
Puga, E. et al. 2004. THE CANTERAS-GALIFA NEOGENE CONGLOMERATES: EVIDENCE FOR AN OPHIOLITIC ASSOCIATION SUBMERGED IN THE MEDITERRANEAN SEA AT THE EASTERN END OF THE BETIC CHAIN. Ofioliti. 29, 2 (Jul. 2004), 213–230. DOI:https://doi.org/10.4454/ofioliti.v29i2.214.