http://www.cnr.it/ontology/cnr/individuo/prodotto/ID43019
Rheological behaviour of the crust in Southern Apennine (Italy): results from a thermal and seismological study (Articolo in rivista)
- Type
- Label
- Rheological behaviour of the crust in Southern Apennine (Italy): results from a thermal and seismological study (Articolo in rivista) (literal)
- Anno
- 2007-01-01T00:00:00+01:00 (literal)
- Alternative label
Solaro G., Tizzani P., Milano G., Pauselli C. (2007)
Rheological behaviour of the crust in Southern Apennine (Italy): results from a thermal and seismological study
in TERRA nova (Print)
(literal)
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- Solaro G., Tizzani P., Milano G., Pauselli C. (literal)
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- Giuseppe Solaro, Girolamo Milano: Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Vesuviano, via Diocleziano, 328 Naples, Italy
Pietro Tizzani: Istituto per il Rilevamento Elettromagnetico dellAmbiente, CNR, via Diocleziano, 328 Naples, Italy
Cristina Pauselli: Dipartimento di Scienze della Terra, Università degli Studi di Perugia, P.zza dellUniversità 1, Perugia, Italy (literal)
- Titolo
- Rheological behaviour of the crust in Southern Apennine (Italy): results from a thermal and seismological study (literal)
- Abstract
- To add information on the brittle/ductile transition of the Southern Apennine, we investigated a rheological profile of the crust along a WSWENE-oriented cross-section running from Neapolitan Volcanic Zone to Apulia foreland. The rheological model was obtained computing a thermal modelling and constrained by a relocalization of earthquakes of the area. Results show that the area is characterized by horizontal rheological variations, with two horizons interlayered with ductile horizons, that are quite predominant with respect to vertical ones. The horizontal stratification of lithospheric rheology has important geodynamic consequence and could provide new insights to better understand the tectonic processes which have played a major role to construct the Southern Apennine belt. Results of this study suggested that well-constrained rheological models, built integrating information from both relocated earthquakes and thermal state, could give important hints on the mechanical behaviour of the crust and its related tectonic processes. (literal)
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