The evolution of He Isotopes in the convecting mantle and the preservation of high He-3/He-4 ratios

A key requirement for any model of mantle evolution is accounting for the high 3He/4He ratios of many ocean island basalts compared to those of mid-ocean ridge basalts. The early, popular paradigm of primitive, undegassed mantle stored in a convectively isolated lower mantle is incompatible with geo...

תיאור מלא

מידע ביבליוגרפי
Main Authors: Porcelli, D, Elliott, T
פורמט: Journal article
שפה:English
יצא לאור: 2008