2013
DOI: 10.1130/g34027.1
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Diffusive helium emissions as a precursory sign of volcanic unrest

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Cited by 78 publications
(63 citation statements)
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“…As shown in previous studies at other sites (e.g., Padrón et al, 2012Padrón et al, , 2013 helium measurements might also work well in the Basin-and-Range Province, since helium is an inert gas and does not react with surrounding rocks, geothermal fluids or groundwater. It could, therefore, be an excellent indicator of a structural connection between deep-seated geothermal reservoirs and surface degassing anomalies.…”
Section: Survey Planning and Optimizationmentioning
confidence: 87%
“…As shown in previous studies at other sites (e.g., Padrón et al, 2012Padrón et al, , 2013 helium measurements might also work well in the Basin-and-Range Province, since helium is an inert gas and does not react with surrounding rocks, geothermal fluids or groundwater. It could, therefore, be an excellent indicator of a structural connection between deep-seated geothermal reservoirs and surface degassing anomalies.…”
Section: Survey Planning and Optimizationmentioning
confidence: 87%
“…Lead-glass sampling bottles with volumes of about 50 cm 3 and with high-vacuum stopcocks at both ends were totally filled with water to sample for dissolved gas. The gas was then extracted by ultrasonic vibration and quantitatively collected into a small volume (10 cm 3 ) following the method described in Padrón et al (2013). The determination of helium isotopic ratios as well as 4 He and 20 Ne concentrations is done following the method described by Sumino et al (2001).…”
Section: Methodsmentioning
confidence: 99%
“…Continuous monitoring of 3 He/ 4 He isotope ratio in diffuse helium flux for forecasting volcanic eruptions could strengthen existing surveillance programs [35]. Standard diffuse degassing methods focus on detecting percolated CO 2 and H 2 S gas as precursors to volcanic eruptions [36].…”
Section: He/ 4 He Ratio Measurements As An Indicator Of Volcanic Unrestmentioning
confidence: 99%