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Helium basalt concentrations

Helium isotope measurements in ocean ridge and island basalts provide some of the most basic geochemical information on mantle source reservoirs. More helium isotope analyses have been performed for oceanic volcanic rocks than for other noble gas species, and helium isotopes have played a leading role in the study of mantle heterogeneity. Helium isotope analyses are readily performed by modern mass spectrometers because there is a general absence of atmospheric contamination in samples due to the low concentration of helium in air (5.24 parts per million by volume at standard temperature and pressure). There are 2 naturally occurring isotopes of helium. He is much less abundant than " He for example, the atmospheric He/" He ratio (Ra) is 1.39x10 (Mamyrin et al. 1970 Clarke et al. 1976). Nearly all of the terrestrial " He has been produced as a-particles from the radioactive decay of U, U and Th over... [Pg.254]


See other pages where Helium basalt concentrations is mentioned: [Pg.992]    [Pg.993]    [Pg.993]    [Pg.2199]    [Pg.2201]    [Pg.2210]    [Pg.3048]    [Pg.291]    [Pg.292]    [Pg.292]    [Pg.263]    [Pg.264]    [Pg.297]    [Pg.354]    [Pg.392]   
See also in sourсe #XX -- [ Pg.309 ]




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