Please use this identifier to cite or link to this item:
192.168.6.56/handle/123456789/2667
Title: | Deep Carbon In Earth |
Authors: | Donato Giovannelli, Giovannelli, Donato |
Keywords: | stastics |
Issue Date: | 2017 |
Publisher: | Frontiers |
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). |
URI: | http://10.6.20.12:80/handle/123456789/2667 |
ISBN: | 978-2-88945-363-4 |
Appears in Collections: | Veterinary Medicine |
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