Antonella AMORUSO | Publications
Antonella AMORUSO Publications
| 2013 | |
| Articolo in rivista | |
| Inversion of synthetic geodetic data for dip-slip faults: clues to theeffects of lateral heterogeneities and data distribution in geologicalenvironments typical of the Apennines (Italy) GEOPHYSICAL JOURNAL INTERNATIONAL. Vol. 192. Pag.745-758 ISSN:1365-246X. | |
| Amoruso, Antonella; Salvatore, Barba; Crescentini, Luca; Antonella, Megna | |
| Digital Object Identifier (DOI): 10.1093/gji/ggs042 Codice identificativo ISI: WOS:000313623100022 Codice identificativo SCOPUS: 2-s2.0-84876818367 | |
| Show it in Product Database (IRIS) |
| 2013 | |
| Articolo in rivista | |
| Global deformations of the Eurasian plate and variations of the Earth rotation rate JOURNAL OF GEODYNAMICS. Vol. 67. Pag.97-105 ISSN:0264-3707. | |
| Vadim, Milyukov; Alexey, Mironov; Vladimir, Kravchuk; Amoruso, Antonella; Crescentini, Luca | |
| Digital Object Identifier (DOI): 10.1016/j.jog.2012.05.009 Codice identificativo ISI: WOS:000318381400012 Codice identificativo SCOPUS: 2-s2.0-84879031333 | |
| Show it in Product Database (IRIS) |
| 2013 | |
| Articolo in rivista | |
| Parsimonious recharge/discharge modeling in carbonate fractured aquifers: The groundwater flow in the Gran Sasso aquifer (Central Italy) JOURNAL OF HYDROLOGY. Vol. 476. Pag.136-146 ISSN:0022-1694. | |
| Amoruso, Antonella; Crescentini, Luca; Marco, Petitta; Marco, Tallini | |
| Digital Object Identifier (DOI): 10.1016/j.jhydrol.2012.10.026 Codice identificativo ISI: WOS:000313861800012 Codice identificativo SCOPUS: 2-s2.0-84871024888 | |
| Show it in Product Database (IRIS) |
| 2013 | |
| Articolo in rivista | |
| Analytical models of volcanic ellipsoidal expansion sources ANNALS OF GEOPHYSICS. Vol. 56. Pag.s0435-1-s0435-19 ISSN:2037-416X. | |
| Amoruso, Antonella; Crescentini, Luca | |
| Digital Object Identifier (DOI): 10.4401/ag-6441 Codice identificativo ISI: WOS:000328254000003 Codice identificativo SCOPUS: 2-s2.0-84887684616 | |
| Show it in Product Database (IRIS) |
