Abstract:

Triassic rift-related volcanic rocks outcrop over all mainland Greece, comprising of trachybasalts and basaltic trachyandesites. Relatively immobile to the effects of alteration processes major and trace element abundances classify the volcanics into OIB and E-MORB lavas. They have mainly been distinguished based upon their: i) LREE contents, ii) silica-saturation index (S·I.), iii) Zr/Nb and Nb/Y ratio values; iv) Th, U, and Ta contents v) geotectonic discrimination diagrams. Their geochemistry indicates that most rocks were affected by moderate to extensive differentiation processes, mostly expressed by clinopyroxene fractionation. Some of the OIB and E-MORB volcanics are considered as primitive undersaturated, displaying (low SiO2, Zr/Nb and S.I. values, enhanced CaO/Al2O3 ratios). Calculated average mantle potential temperatures are comparable (1410 °C OIB; 1370 °C E-MORB), with melt fractions estimated at 3–5% for primary OIB magmas and 6–8% for primary E-MORB magmas. An asthenospheric origin is inferred for the OIB lavas, with melting in the garnet stability field (75–95 km; 2.5–3.0 GPa), whereas E-MORB parent magmas were formed with melting in the garnet/spinel (transitional) stability field (55–70 km; 1.8–2.2 GPa). The Hellenic Triassic rift-related lavas were most likely generated and erupted after lithospheric attenuation and extension, followed by subsequent asthenospheric upwelling of the mantle. The high calculated partial melting degrees and the observed thick and voluminous lava formations account for fast-spreading of the Tethys ridge during the Triassic. Temperature results suggest that the Hellenic Triassic rift-related magmas were generated from mantle at ambient temperature, render a mantle plume-based scenario improbable.