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- W2355557133 abstract "CO_2 is the main gas component derived from magma at the dormant volcanic regions in China,and the volume percentage contents range from 80% to 99%.The micro gases studied here are CH_4,He,H_2,N_2,Ar,O_2,H_2S,SO_2,CO etc.,the CH_4 and He among them are the most important gas components derived from the mantle magma.The 3He/4He ratio is the most reliable indicator of the mantle matter; and also the distinctive carbon isotopic compositions(δ~(13)C)of CO_2 and CH_4 derived from magma distinguish from the shallow gases.In the Tianchi volcanic area,Changbai Mountains,the monitoring results about the carbon isotopic fractionation between the CO_2 and CH_4 suggest that the local mantle magma disturbance happened,following Wangqing Ms 7.2 deep-seated earthquake on June 29,2002,but a large-scale upwelling mantle material would be not occurred.This fact means that there is not immediate volcano eruption danger at the studied area." @default.
- W2355557133 created "2016-06-24" @default.
- W2355557133 creator A5046793688 @default.
- W2355557133 date "2008-01-01" @default.
- W2355557133 modified "2023-09-25" @default.
- W2355557133 title "Geochemical features of magmatic gases in the regions of dormant volcanoes in China." @default.
- W2355557133 hasPublicationYear "2008" @default.
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