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- W2019156949 abstract "[1] We report new He and CO2 data for geothermal fluids from Changbaishan Volcano located on the border of China and North Korea. Helium isotope ratios reach a maximum of 5.4 RA (where RA = 3He/4He in air) whereas carbon isotope values (δ13C) fall between −2 and −7 ‰ (vs. PDB). The ratio of CO2/3He varies between 0.5–7.1 (×109) for gas samples but is considerably higher (∼1012) in waters. The combined He-CO2 systematics reveal the clear imprint of a dominant subducted slab contribution to the total CO2 inventory. We conclude that these geothermal volatiles originate from the sub-continental lithospheric mantle (SCLM) in NE China and represent ancient fluids captured by prior metasomatic events." @default.
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- W2019156949 date "2008-11-25" @default.
- W2019156949 modified "2023-09-29" @default.
- W2019156949 title "Geothermal He and CO<sub>2</sub>variations at Changbaishan intra-plate volcano (NE China) and the nature of the sub-continental lithospheric mantle" @default.
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