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- W2073167220 abstract "Mapping and characterizing fracturing in a volcanic terrain is facilitated by the analysis of physical and chemical properties of soils. The parameters analyzed include the temperature at shallow depth, the spontaneous potential (SP), and the 4He, 44CO2, and 222Rn contents of soil gases, as measured in situ by mass spectrometry and α counter. This analysis allowed a distinction of deep fissures not accompanied by thermal loss, characterized by a negative SP anomaly and high He levels, and of a hidden fissure with thermal loss, characterized by a positive SP anomaly and high He, Rn, and CO2 levels. This fissure has no visible surface manifestations. This method of analysing the convective thermal transfer is useful when analysing fracturing in volcanic structures to estimate their eruptive potential." @default.
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- W2073167220 date "1988-11-01" @default.
- W2073167220 modified "2023-09-24" @default.
- W2073167220 title "Identification of a hidden thermal fissure in a volcanic terrain using a combination of hydrothermal convection indicators and soil-atmosphere analysis" @default.
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- W2073167220 doi "https://doi.org/10.1016/0377-0273(88)90018-2" @default.
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