Deep Carbon In Earth

dc.contributor.author	Donato Giovannelli,	en
dc.contributor.editor	Giovannelli, Donato
dc.date.accessioned	2018-09-19T09:21:18Z
dc.date.accessioned	2023-07-20T09:11:52Z
dc.date.available	2018-09-19T09:21:18Z
dc.date.available	2023-07-20T09:11:52Z
dc.date.issued	2017
dc.identifier.isbn	978-2-88945-363-4
dc.identifier.uri	http://10.215.13.25/handle/123456789/2667
dc.description	Carbon 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.language	en	en
dc.language.iso	en	en_US
dc.publisher	Frontiers	en_US
dc.subject	stastics	en_US
dc.title	Deep Carbon In Earth	en_US
dc.type	Book	en_US