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- W2076372425 abstract "Temporal variations of 3He4HE and 4He20Ne ratios occur in high-temperature gases from a steam well located about 3 km north of the central cone of Mt. Mihara, an active volcano in Oshima Island, Japan. The 3He4He ratio gradually increased from 1.71Ratm (1.71 times the atmospheric ratio of 1.40 × 10−6) in October 1986 to 5.02.Ratm in November 1987. Taking into account a similar 4He20Ne change, the magmatic He component in the steam has increased since the violent eruptions of Oshima volcano from November 15 to December 18, 1986. This confirms a direct relationship between magmatic activity and elevated 3He4He ratios in groundwater/hydrothermal systems. Based on the distance from the craters to the steam well, the time lag between the eruptions, and the increase of 3He4He, we estimate the magmatic component velocity in the fluid flow. The calculated value, several tens of m per day, is significantly higher than typical groundwater flow in deep sedimentary basins of Japan." @default.
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- W2076372425 date "1988-05-01" @default.
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- W2076372425 title "Influence of volcanic eruptions on helium isotope ratios in hydrothermal systems induced by volcanic eruptions" @default.
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- W2076372425 doi "https://doi.org/10.1016/0016-7037(88)90284-0" @default.
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