Zobrazeno 1 - 2
of 2
pro vyhledávání: '"Doglioni C.(1)"'
Publikováno v:
Earth and planetary science letters 450 (2016): 292–305. doi:10.1016/j.epsl.2016.06.042
info:cnr-pdr/source/autori:Smeraglia L.[1], Berra F.[2], Billi A.[3], Boschi C.[4], Carminati E.[1,3], Doglioni C.[1,3]/titolo:Origin and role of fluids involved in the seismic cycle of extensional faults in carbonate rocks./doi:10.1016%2Fj.epsl.2016.06.042/rivista:Earth and planetary science letters/anno:2016/pagina_da:292/pagina_a:305/intervallo_pagine:292–305/volume:450
info:cnr-pdr/source/autori:Smeraglia L.[1], Berra F.[2], Billi A.[3], Boschi C.[4], Carminati E.[1,3], Doglioni C.[1,3]/titolo:Origin and role of fluids involved in the seismic cycle of extensional faults in carbonate rocks./doi:10.1016%2Fj.epsl.2016.06.042/rivista:Earth and planetary science letters/anno:2016/pagina_da:292/pagina_a:305/intervallo_pagine:292–305/volume:450
We examine the potentially-seismic right-lateral transtensional-extensional Tre Monti Fault (central Apennines, Italy) with structural and geochemical methods and develop a conceptual evolutionary model of extensional faulting with fluid involvement
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::057a49f4c77dba13454b57610faee43d
https://doi.org/10.1016/j.epsl.2016.06.042
https://doi.org/10.1016/j.epsl.2016.06.042
Publikováno v:
Flooding and Environmental Challenges for Venice and its Lagoon, edited by C. Fletcher & T. Spencer, pp. 21–28. Cambridge: Cambridge University Press, 2005
info:cnr-pdr/source/autori:Carminati E.(1), Doglioni C.(1), Scrocca D.(2)/titolo:Magnitude and causes of long-term subsidence of the Po Plain and Venetian region/titolo_volume:Flooding and Environmental Challenges for Venice and its Lagoon/curatori_volume:C. Fletcher & T. Spencer/editore: /anno:2005
info:cnr-pdr/source/autori:Carminati E.(1), Doglioni C.(1), Scrocca D.(2)/titolo:Magnitude and causes of long-term subsidence of the Po Plain and Venetian region/titolo_volume:Flooding and Environmental Challenges for Venice and its Lagoon/curatori_volume:C. Fletcher & T. Spencer/editore: /anno:2005
In the Po Plain (Northern Italy), the natural component of subsidence can be split into: (1) a long-term component controlled by tectonics and geodynamics, active on time periods of about 106 yr; (2) a shortterm component, controlled by climatic chan
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::0270a776532ecdb9e6ac1d06caccac58
https://publications.cnr.it/doc/135573
https://publications.cnr.it/doc/135573
