Zobrazeno 1 - 10
of 153
pro vyhledávání: '"F. Galadini"'
Publikováno v:
Solid Earth, Vol 9, Pp 911-922 (2018)
We investigated the eastern corner of northeastern Italy, where a system of NW–SE-trending dextral strike-slip faults of western Slovenia intersects the south-verging fold and thrust belt of the eastern Southern Alps. The area suffered the large
Externí odkaz:
https://doaj.org/article/4da0ba8c648a41a38f3a3d7668b9bc05
Publikováno v:
Solid Earth, Vol 8, Iss 2, Pp 319-337 (2017)
The general basin and range Apennine topographic characteristic is generally attributed to the presently active normal fault systems, whose long-term activity (throughout the Quaternary) is supposed to have been responsible for the creation of morpho
Externí odkaz:
https://doaj.org/article/cd3b982fccd2415683950a774b420608
Autor:
P. Galli, F. Galadini
Publikováno v:
Annals of Geophysics, Vol 47, Iss 2-3 (2004)
The 346 A.D. earthquake is known through sparse historical sources. It is mentioned by Hyeronimus as felt in Rome and responsible for damage in the ancient Campania Province. Four epigraphs report the earthquake as the cause for the restorations of b
Externí odkaz:
https://doaj.org/article/767a51e3b8fe41e5a3ece378c66d1a05
Publikováno v:
Annals of Geophysics, Vol 46, Iss 5 (2003)
Paleoseismological analyses were performed along the Campo Imperatore Fault (part of the Gran Sasso Range Fault System) in order to define the seismogenic behaviour (recurrence interval for surface faulting events, elapsed time since the last activ
Externí odkaz:
https://doaj.org/article/5f63d5ee4d8a4a498ab084f6bc1534d2
Autor:
P. Galli, F. Galadini
Publikováno v:
Annals of Geophysics, Vol 46, Iss 5 (2003)
Paleoseismological analyses have been performed in the Central Apennines along faults showing geomorphological evidence of Late Quaternary activity and characterised by the absence of historical seismicity. Three trenches were made along the Mt. Ve
Externí odkaz:
https://doaj.org/article/5f14d238967d4b939b40926da375e7f7
Autor:
P. Galli, F. Galadini
Publikováno v:
Annals of Geophysics, Vol 39, Iss 5 (1996)
During paleoseismological investigations on the seismogenic structure responsible for the 1915 earthquake in the Fucino Plain (Central Italy), some trenches were excavated at the intersection between Roman-age channels and a fault characterized by Ho
Externí odkaz:
https://doaj.org/article/d3defe0760e44b30b3856a67ce9a7333
Publikováno v:
Annals of Geophysics, Vol 38, Iss 3-4 (1995)
The paleomagnetism of the Plio-Pleistocene continental sediments cropping out at the north-eastern edge of the Fucino extensionaI basin (Italy, Central Apennines) was investigated. The area is characterized by strong neo-tectonic activity and the ori
Externí odkaz:
https://doaj.org/article/25284e15440144d38b9700576bf068e2
Autor:
R. Giuliani, F. Galadini
Publikováno v:
Annals of Geophysics, Vol 36, Iss 1 (1993)
Externí odkaz:
https://doaj.org/article/8fa5d7233bf94d73b1fcfb3c6dfc037b
Autor:
P. Messina, F. Galadini
Publikováno v:
Annals of Geophysics, Vol 36, Iss 1 (1993)
Externí odkaz:
https://doaj.org/article/65dba8ed70954182bc670b1a1a239297
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