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- W1999941644 abstract "We examine models for batch-equilibrium and fractional-equilibrium degassing of CO2 from magma at Kilauea Volcano. The models are based on (1) the concept of two-stage degassing of CO2 from magma supplied to the summit chamber, (2) C isotope data for CO2 in eruptive and noneruptive (quiescent) gases from Kilauea and (3) data for the isotopic fractionation of C between CO2 and C dissolved in tholeiitic basalt melt. (1) both eruptive and noneruptive degassing of CO2 most closely approach a batch equilibrium process, (2) the δ13C of parental magma supplied to the summit chamber is in the range −4.1 to−3.4‰ and (3) the δ13C of melt after summit chamber degassing is in the range −7 to −8‰, depending upon the depth of equilibration." @default.
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- W1999941644 date "1990-07-01" @default.
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- W1999941644 title "Carbon isotope constraints on degassing of carbon dioxide from Kilauea Volcano" @default.
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- W1999941644 doi "https://doi.org/10.1016/0016-7037(90)90270-u" @default.
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