作者: S. Esperança , G. M. Crisci , R. de Rosa , R. Mazzuoli
DOI: 10.1007/BF00310777
关键词:
摘要: Volcanic rocks on the island of Lipari show entire range Sr, Nd, Pb isotopic compositions displayed by other islands in Aeolian archipelago. The rapid evolution subaerial volcanic towards crustal values together with appropriate composition neighbouring Calabrian crust (Serre) indicate that many geochemical characteristics observed lavas can be attributed to contamination and mixing materials melts. Interpretation data is complicated fact underplating onto crust-mantle boundary specific lithologies present section differ underneath each individual sector island. In central northern parts island, metapelitic were incorporated provide more radiogenic Sr some lavas. products from M. Guardia southern part Lipari, where activity restricted last 30–40 ka, bear similarities Vulcano, it proposed considerable remobilization took place presence mafic mantle-derived On petrogenetic processes magma assimilation dominate over fractional crystallization, increase K2O Na2O correlated contributions lithologies. It suggested variability budget alkalis (Na2O versus K2O) explained invoking a heat source an intruding asthenospheric MORB-type mantle into cooler lithospheric crust/mantle during opening Tyrrhenian basin.