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They may be part of a layered oceanic complex. The REE distributions in the residual liquids left after such a fractionation are similar to those of incompatible element-depleted oceanic tholeiites. The REE data indicate that the basalts which overlie the gabbro-peridotite complex, are not genetically related to plutonic rocks.","descriptionType":"Abstract"},{"description":"Supplement to: Dostal, J; Muecke, G K (1978): Trace element geochemistry of the peridotite-gabbro-basalt suite from DSDP Leg 37. Earth and Planetary Science Letters, 40(3), 415-422","descriptionType":"Other"}],"geoLocations":[{"geoLocationPoint":{"pointLatitude":"37.035500000000006","pointLongitude":"-34.41449999999999"}},{"geoLocationPlace":"North 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