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Basalts neon isotopes

Dodson, A., Kennedy, B. M., DePaolo, D. J. (1997) Helium and neon isotopes in the Imnaha basalt, Columbia River Basalt Group Evidence for a Yellowstone plume source. Earth Planet. Sci. Lett., 150, 443-51. [Pg.258]

Poreda, R., Radicati di Brozolo, F. (1984) Neon isotope variations in Mid-Atlantic Ridge basalts. Earth Planet. Sci. Lett., 69, 277-89. [Pg.272]

Dixon E. T., Honda M., McDougall 1., Campbell 1. H., and Sigurdsson 1. (2000) Preservation of near-solar neon isotopic ratios in Icelandic basalts. Earth Planet. Sci. Lett. 180, 309 - 324. [Pg.545]

Sarda P., Staudacher T., and Allegre C. J. (1988) Neon isotopes in submarine basalts. Earth Planet. Sci. Lett. 91, 73-88. [Pg.1017]

Dixon ET (2002) Interpretation of helium and neon isotopic heterogeneity in Icelandic basalts. Earth Planet Sci Lett (submitted)... [Pg.471]

Dixon JE, Stolper EM (1995) An experimental study of water and carbon dioxide solubihties in mid-ocean ridge basaltic liquids. 2. Applications to degassing. J Petrol 36 1633-1646 Dixon ET, Honda M, McDougall I, Campbell IH, Sigurdsson I (2000) Preservation of near-solar neon isotopic ratios in Icelandic basalts. Earth Planet Sci Lett 180 309-324 Doe BR, Zartman RE (1979) Plumbotectonics I. the Phanerozoic. In Geochemistry of hydrothermal ore deposits. Bames HL (ed) Wiley, New York, p 22-70... [Pg.471]

Figure 3 The distribution of neon isotopes in mantle-derived rocks, indicating the presence of an atmospheric component, a radiogenic component adding Ne (produced by neutrons from uranium fission acting on oxygen and magnesium), and a solar component. It is this latter that indicates that gases in the mantle were derived from the capture of solar material in the early history of the Earth. M = MORB (midocean ridge basalts) P = plume or ocean island basalts (OIB) A = atmosphere. Solar neon is represented by the horizontal line at Ne/ Ne = 12.5 MFL is the mass fractionation line. The presence of solar neon in ocean basalts was first identified by Craig and Lupton (Craig H and Lupton JE (1976) Earth and Planetary Science Letters 31 369-385). (Reprinted with permission from Farley and Poreda (1993). Figure 3 The distribution of neon isotopes in mantle-derived rocks, indicating the presence of an atmospheric component, a radiogenic component adding Ne (produced by neutrons from uranium fission acting on oxygen and magnesium), and a solar component. It is this latter that indicates that gases in the mantle were derived from the capture of solar material in the early history of the Earth. M = MORB (midocean ridge basalts) P = plume or ocean island basalts (OIB) A = atmosphere. Solar neon is represented by the horizontal line at Ne/ Ne = 12.5 MFL is the mass fractionation line. The presence of solar neon in ocean basalts was first identified by Craig and Lupton (Craig H and Lupton JE (1976) Earth and Planetary Science Letters 31 369-385). (Reprinted with permission from Farley and Poreda (1993).
Weaver BL (1991) Trace element evidence for the origin of ocean-island basalts. Geology 19 123-126 Wetherill GW (1954) Variations in the isotopic abundances of neon and argon extracted from radioactive minerals. Phys Rev 96 679-683... [Pg.318]

See other pages where Basalts neon isotopes is mentioned: [Pg.989]    [Pg.989]    [Pg.991]    [Pg.1010]    [Pg.219]    [Pg.288]    [Pg.288]    [Pg.290]    [Pg.309]    [Pg.307]    [Pg.313]    [Pg.318]    [Pg.364]    [Pg.461]    [Pg.869]    [Pg.173]    [Pg.989]    [Pg.2210]    [Pg.288]    [Pg.189]    [Pg.284]    [Pg.316]    [Pg.316]   
See also in sourсe #XX -- [ Pg.287 , Pg.288 , Pg.289 ]



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