Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Jarðhitakerfi"'
Publikováno v:
Geofluids, Vol 2019 (2019)
Publisher's version
Supercritical fluids exist in the roots of many active high-temperature geothermal systems. Utilization of such supercritical resources may multiply energy production from geothermal systems; yet, their occurrence, formation
Supercritical fluids exist in the roots of many active high-temperature geothermal systems. Utilization of such supercritical resources may multiply energy production from geothermal systems; yet, their occurrence, formation
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::86a8495771296ca058b4b740f2a4e3e9
https://doi.org/10.1155/2019/6023534
https://doi.org/10.1155/2019/6023534
Publikováno v:
Nature Communications, Vol 11, Iss 1, Pp 1-11 (2020)
Publisher's version (útgefin grein)
Glacier runoff and melt from volcanic and geothermal activity accumulates in glacier dammed lakes in glaciated areas around the world. These lakes eventually drain, creating hazardous subglacial floods that a
Glacier runoff and melt from volcanic and geothermal activity accumulates in glacier dammed lakes in glaciated areas around the world. These lakes eventually drain, creating hazardous subglacial floods that a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::dbe805bf458cb30111e71228bf74ee18
https://doi.org/10.1038/s41467-020-15744-5
https://doi.org/10.1038/s41467-020-15744-5
Autor:
Concetta Rispoli, Carla Grimaldi, Tobias B. Weisenberger, Kristján Jónasson, Marie D. Jackson, Piergiulio Cappelletti, Magnús T. Gudmundsson, Simon Prause
The evolution of hydrothermal alteration in glassy and variably palagonitized tuff, erupted as tephra in 1963 – 1964 on Surtsey, an island built in the offshore extension of Iceland’s southeast rift zone, is documented through a comparative petro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e633e9463cdc97e406531e00f5f838f1
http://hdl.handle.net/11588/786965
http://hdl.handle.net/11588/786965
Autor:
Freysteinn Sigmundsson, Benoit Gibert, Ólafur G. Flóvenz, Pierre Briole, Léa Lévy, Philippe Pezard, Gylfi Páll Hersir
Publikováno v:
Geophysical Journal International
Geophysical Journal International, Oxford University Press (OUP), 2018, 215 (3), pp.1558-1582. ⟨10.1093/gji/ggy342⟩
Geophysical Journal International, Oxford University Press (OUP), 2018, 215 (3), pp.1558-1582. ⟨10.1093/gji/ggy342⟩
Publisher's version (útgefin grein)
The underground circulation of hot water, of interest for geothermal energy production, is often indirectly inferred from the presence of minerals formed by hydrothermal alteration at different temperatures.
The underground circulation of hot water, of interest for geothermal energy production, is often indirectly inferred from the presence of minerals formed by hydrothermal alteration at different temperatures.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d37adfac58fcf45005a4ebcf73b2f085
https://hal.umontpellier.fr/hal-02071793
https://hal.umontpellier.fr/hal-02071793
Liquid dominated reservoirs are a common type of hydrothermal reservoirs. They consist of fractured rock and reservoir fluid which may obey Darcy’s law. Steam can form in such reservoirs either through heat input which causes temperature increase o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3712::8469a712de8e05bfafb94e8788685cc2
https://hdl.handle.net/20.500.11815/1188
https://hdl.handle.net/20.500.11815/1188