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Interpretation of radon anomalies in seismotectonic and tectono-gravitational analyses: the SE portion of the Crati graben (Northern Calabria, Italy). (Articolo in rivista)
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- Interpretation of radon anomalies in seismotectonic and tectono-gravitational analyses: the SE portion of the Crati graben (Northern Calabria, Italy). (Articolo in rivista) (literal)
- Anno
- 2005-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1016/j.tecto.2004.11.008 (literal)
- Alternative label
TANSI C. (1); TALLARICO A. (2); IOVINE G. (1); FÒLINO-GALLO M. (1); FALCONE G. (2) (2005)
Interpretation of radon anomalies in seismotectonic and tectono-gravitational analyses: the SE portion of the Crati graben (Northern Calabria, Italy).
in Tectonophysics (Amst. Online); ELSEVIER, NEW YORK (Stati Uniti d'America)
(literal)
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- TANSI C. (1); TALLARICO A. (2); IOVINE G. (1); FÒLINO-GALLO M. (1); FALCONE G. (2) (literal)
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- Elsevier, ISSN: 0040-1951. Impact Factor: 1.732 (2005) cfr. Journal Citation Reports®, Published by Thomson Reuters - ISI WoS
VQR 2004/2010 = 0.8
ISI WoS: 000227112200004
Scopus: 2-s2.0-13644278198
SCImago SJR (2006) = 1,602 - Subject Category: Earth-Surface Processes: Q1
DOI: 10.1016/j.tecto.2004.11.008 - URL: http://www.sciencedirect.com/science/article/pii/S0040195104004846
G-Scholar: http://www.sciencedirect.com/science/article/pii/S0040195104004846 - http://scholar.google.it/scholar?oi=bibs&hl=it&cluster=2588030213134893906
Numero di citazioni = 27 al 21 ott. 2013 - fonte: G-Scholar
Numero di citazioni = 22 al 21 ott. 2013 - fonte: WoS
Numero di citazioni = 21 al 21 ott. 2013 - fonte: Scopus
Impact Factor: 2.684 (2012) cfr. Journal Citation Reports®, Published by Thomson Reuters - ISI WoS (literal)
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- http://www.sciencedirect.com/science/article/pii/S0040195104004846 (literal)
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- 1) CNR-IRPI UOS di Cosenza
2) Unical - Dip. Fisica (literal)
- Titolo
- Interpretation of radon anomalies in seismotectonic and tectono-gravitational analyses: the SE portion of the Crati graben (Northern Calabria, Italy). (literal)
- Abstract
- The study area is located in the south-eastern part of the Crati valley (Northern Calabria, Italy), which is a graben bordered
by N-S trending normal faults and crossed by NW-SE normal left-lateral faults. Numerous severe crustal earthquakes have
affected the area in historical time. Present-day seismic activity is mainly related to the N-S faults located along the eastern
border of the graben. In this area, much seismically induced deep-seated deformation has also been recognised.
In the present paper, radon concentrations in soil gas have been measured and compared with (a) lithology, (b) Quaternary
faults, (c) historical and instrumental seismicity, and (d) deep-seated deformation.
The results highlight the following:
(a) There is no evidence of a strong correlation between lithology and the radon anomalies.
(b) A clear correlation between the N-S geometry of radon anomalies and the orientation of main fault systems has been
recognised, except in the southernmost part of the area, where the radon concentrations are strongly affected by the
superposition of the N-S and the NW-SE fault systems.
(c) Epicentral zones of instrumental and historical earthquakes correspond to the highest values of radon concentrations,
probably indicating recent activated fault segments. In particular, high radon values occur in the zones struck by
earthquakes in 1835, 1854, and 1870.
(d) Deep-seated gravitational deformation generally coincides with zones characterised by low radon concentrations. (literal)
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