Please use this identifier to cite or link to this item: 192.168.6.56/handle/123456789/2667
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dc.contributor.authorDonato Giovannelli,en
dc.contributor.editorGiovannelli, Donato-
dc.date.accessioned2018-09-19T09:21:18Z-
dc.date.available2018-09-19T09:21:18Z-
dc.date.issued2017-
dc.identifier.isbn978-2-88945-363-4-
dc.identifier.urihttp://10.6.20.12:80/handle/123456789/2667-
dc.descriptionCarbon dioxide (CO2) together with water vapor (H2O) and sulfur dioxide (SO2) are usually the most abundant gases released to the atmosphere during volcanic eruptions (Giggenbach, 1996; Fischer and Chiodini, 2015 and references therein). During non-eruptive periods, gas emissions are also frequent in many volcanic systems not only through the presence of permanent fumaroles, but also due to the existence of thermal and cold CO2-rich springs, as well as soil diffuse degassing emissions (Allard et al., 1991; Chiodini et al., 1998).en
dc.languageenen
dc.language.isoenen_US
dc.publisherFrontiersen_US
dc.subjectstasticsen_US
dc.titleDeep Carbon In Earthen_US
dc.typeBooken_US
Appears in Collections:Veterinary Medicine

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