Enhanced 3He 4He ratios and cosmogenic helium in ultramafic xenoliths

Recently erupted ultramafic xenoliths generally have ratios of 3He 4He = (5-10) × RA, which are similar to the values characterizing mid-ocean ridge basalts (MORB). During the course of additional investigations of ultramafic xenoliths, samples from several locations have been found with 3He 4He r...

Πλήρης περιγραφή

Λεπτομέρειες βιβλιογραφικής εγγραφής
Κύριοι συγγραφείς: Porcelli, DR, Stone, J, O'Nions, R
Μορφή: Journal article
Γλώσσα:English
Έκδοση: 1987