Zobrazeno 1 - 2
of 2
pro vyhledávání: '"Magro G. (3)"'
Publikováno v:
Proceedings 5th African Rift Geothermal Conference, Arusha, Tanzania, 29-31 October 2014
info:cnr-pdr/source/autori:Montegrossi G.[1], Ruggieri G.[1], Pasqua C., Magro G.[3]/congresso_nome:Proceedings 5th African Rift Geothermal Conference/congresso_luogo:Arusha, Tanzania/congresso_data:29-31 October 2014/anno:2014/pagina_da:/pagina_a:/intervallo_pagine
info:cnr-pdr/source/autori:Montegrossi G.[1], Ruggieri G.[1], Pasqua C., Magro G.[3]/congresso_nome:Proceedings 5th African Rift Geothermal Conference/congresso_luogo:Arusha, Tanzania/congresso_data:29-31 October 2014/anno:2014/pagina_da:/pagina_a:/intervallo_pagine
The Tendaho geothermal system is characterized by the presence of a 50 km wide graben trending NW- SE, dissected on its turn by a series of normal faults which form a sequence of secondary horst and graben. The graben basement is composed of fissural
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::382d169aa9a596b424781cc6a448292b
http://theargeo.org/argeoc5.html
http://theargeo.org/argeoc5.html
Autor:
Vaselli O. (1, Minissale A. (2), Tassi F. (1), Magro G. (3), Seghedi I. (4), Ioane D.(4), Szakacs A. (4)
Publikováno v:
Chemical geology 182 (2002): 637–654. doi:10.1016/S0009-2541(01)00348-5
info:cnr-pdr/source/autori:Vaselli O. (1,2), Minissale A. (2), Tassi F. (1), Magro G. (3), Seghedi I. (4), Ioane D.(4), Szakacs A. (4)/titolo:A geochemical traverse across the eastern Carpathians (Romania): Constraints on the origin and evolution of the mineral water and gas discharges./doi:10.1016%2FS0009-2541(01)00348-5/rivista:Chemical geology/anno:2002/pagina_da:637/pagina_a:654/intervallo_pagine:637–654/volume:182
info:cnr-pdr/source/autori:Vaselli O. (1,2), Minissale A. (2), Tassi F. (1), Magro G. (3), Seghedi I. (4), Ioane D.(4), Szakacs A. (4)/titolo:A geochemical traverse across the eastern Carpathians (Romania): Constraints on the origin and evolution of the mineral water and gas discharges./doi:10.1016%2FS0009-2541(01)00348-5/rivista:Chemical geology/anno:2002/pagina_da:637/pagina_a:654/intervallo_pagine:637–654/volume:182
The inner sector of the Eastern Carpathians displays a large number of Na–HCO 3 , CO 2 -rich, meteoric-originated cold springs (soda springs) and bore wells, as well as dry mofettes. They border the southern part of the Pliocene–Quaternary Calima
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d26b33a1b89fea05e50390a1e24015c5
https://publications.cnr.it/doc/29124
https://publications.cnr.it/doc/29124