Zobrazeno 1 - 4
of 4
pro vyhledávání: '"J. D. Rogie"'
Autor:
William C. Evans, Ben Kennedy, David A. Stonestrom, Michael L. Sorey, J. D. Rogie, David L. Shuster
Publikováno v:
Chemical Geology. 177:15-29
Diffuse emissions of CO2 are known to be large around some volcanoes and hydrothermal areas. Accumulation-chamber measurements of CO2 flux are increasingly used to estimate the total magmatic or metamorphic CO2 released from such areas. To assess the
Publikováno v:
Earth and Planetary Science Letters. 188:535-541
Mammoth Mountain, a dormant volcano in the eastern Sierra Nevada, California, has been passively degassing large quantities of cold magmatic CO2 since 1990 following a 6-month-long earthquake swarm associated with a shallow magmatic intrusion in 1989
Autor:
Francesco Parello, Francesco Frondini, A.R. Zanzari, Derrill M. Kerrick, L. Peruzzi, J. D. Rogie, Giovanni Chiodini
In Central Italy non-volcanic CO 2 is discharged by focused degassing (strong diffuse emission and vents) and by high-CO 2 groundwater. 3 He / 4 He data and the carbon isotopic composition of CO 2 are compatible with derivation from mantle degassing
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::744042288c8d883d3f94edc1bb90f0bc
http://hdl.handle.net/11391/163823
http://hdl.handle.net/11391/163823
Publikováno v:
Scopus-Elsevier
In central Italy, nonvolcanic CO2 is discharged from many areas of focused degassing (vents and associated strong diffuse emission) and from high-pCO2 groundwater. We estimate that there are at least 100 CO2 vents in central Italy, many of which have
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4bc453350e2570b7ac797483a4c02a3e
http://www.scopus.com/inward/record.url?eid=2-s2.0-0034629838&partnerID=MN8TOARS
http://www.scopus.com/inward/record.url?eid=2-s2.0-0034629838&partnerID=MN8TOARS