Seismic evidence for a low-velocity zone in the upper crust beneath mount vesuvius
- Autor
- ZOLLO, A1 ; GASPARINI, P1 ; DE MATTEIS, R; GUERRA, I7 ; LANNACCONE, G1 ; MIRABILE, L8 ; VILARDO, G4 ; VIRIEUX, J2 ; LE MEUR, H; DE NATALE, G4 ; BIELLA, G5 ; BOSCHI, E6 ; CAPUANO, P4 ; DE FRANCO, R5 ; DELL'AVERSANA, P1
Dipartimento de Geofisica e Vulcanologia, Università di Napoli Federico II, Largo S. marcellino 10, 80138, Italy
[1] Dipartimento di Geofisica e Vulcanologia, Università di Napoli Federico II, largo S. Marcellino 10, 80138 Napoli, Italy
[2] Institut de Géodynamique, CNRS Sophia-Antipolis, France
[4] Osservatorio Vesuviano, Napoli, Italy
[5] instituto per le Richerche sul Rischio Sismico, Consiglio Nazionale delle Ricerche (CNR), Milano, Italy
[6] Instituto Nazionale di Geofisica, Roma, Italy
[7] Dipartimento di Scienze della Terra, Università della Calabria, Cosenza, Italy
[8] Instituto di Oceanologia, Instituto Universitario Navale, Napoli, Italy - Fuente
Science (Washington, D.C.). 1996, Vol 274, Num 5287, pp 592-594 ; Illustration
- CODEN
- SCIEAS
- ISSN
- 0036-8075
- Campo Científico
- Multidisciplinary
- Editor
- American Association for the Advancement of Science, Washington, DC
- País de la publicación
- United States
- Tipo de documento
- Article
- Idioma
- English
- Palabra clave (fr)
- Chambre magmatique Croûte terrestre sup Matière fondue Microséisme Modèle 2 dimensions Mésozoïque Onde P Onde S Onde sismique Profil sismique Roche carbonatée Réseau sismique Sismique réflexion Socle Stratovolcan Structure vitesse Temps arrivée Tomographie Tracé rayon Volcan Vésuve Europe Phanérozoïque Roche sédimentaire Campanie Europe Sud Italie
- Palabra clave (in)
- magma chambers upper crust melts microseisms two-dimensional models Mesozoic P-waves S-waves seismic waves seismic profiles carbonate rocks seismic networks seismic reflection basement stratovolcanoes velocity structure arrival time tomography ray tracing Vesuvius Europe Phanerozoic sedimentary rocks Campania Italy Southern Europe Italy
- Palabra clave (es)
- Cámara magmática Corteza terrestre sup Producto fundido Microsismo Modelo 2 dimensiones Onda P Onda S Onda sísmica Roca carbonatada Red sísmica Método reflexión sísmica Basamento Estratovolcán Estructura velocidad Tiempo llegada Tomografía Volcán Vesuvio Europa Fanerozoico Roca sedimentaria Campania Europa Sur Italia
- Clasificación
- Pascal
- 001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01F Crystalline rocks / 001E01F01 Igneous and metamorphic rocks petrology, volcanic processes, magmas
- Pascal
- 001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences / 001E01M Internal geophysics / 001E01M03 Earthquakes, seismology
- Disciplina
- Earth sciences
- Procedencia
- Inist-CNRS
- Base de datos
- PASCAL
- Identificador INIST
- 2484825
Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS
Install on your browser
"O:13:\"PanistOpenUrl\":36:{s:10:\"\u0000*\u0000openUrl\";N;s:6:\"\u0000*\u0000idc\";N;s:6:\"\u0000*\u0000fmt\";s:7:\"journal\";s:6:\"\u0000*\u0000doi\";s:0:\"\";s:6:\"\u0000*\u0000pii\";s:0:\"\";s:7:\"\u0000*\u0000pmid\";s:0:\"\";s:9:\"\u0000*\u0000atitle\";s:82:\"Seismic evidence for a low-velocity zone in the upper crust beneath mount vesuvius\";s:9:\"\u0000*\u0000jtitle\";s:26:\"Science (Washington, D.C.)\";s:9:\"\u0000*\u0000stitle\";s:20:\"Science (Wash. D.C.)\";s:7:\"\u0000*\u0000date\";s:4:\"1996\";s:9:\"\u0000*\u0000volume\";s:3:\"274\";s:8:\"\u0000*\u0000issue\";s:4:\"5287\";s:8:\"\u0000*\u0000spage\";s:3:\"592\";s:8:\"\u0000*\u0000epage\";s:3:\"594\";s:8:\"\u0000*\u0000pages\";s:0:\"\";s:7:\"\u0000*\u0000issn\";s:9:\"0036-8075\";s:8:\"\u0000*\u0000eissn\";s:0:\"\";s:9:\"\u0000*\u0000aulast\";s:5:\"ZOLLO\";s:10:\"\u0000*\u0000aufirst\";s:1:\"A\";s:9:\"\u0000*\u0000auinit\";s:0:\"\";s:10:\"\u0000*\u0000auinitm\";s:0:\"\";s:5:\"\u0000*\u0000au\";a:14:{i:0;s:12:\"GASPARINI, P\";i:1;s:13:\"DE MATTEIS, R\";i:2;s:9:\"GUERRA, I\";i:3;s:13:\"LANNACCONE, G\";i:4;s:11:\"MIRABILE, L\";i:5;s:10:\"VILARDO, G\";i:6;s:10:\"VIRIEUX, J\";i:7;s:10:\"LE MEUR, H\";i:8;s:12:\"DE NATALE, G\";i:9;s:9:\"BIELLA, G\";i:10;s:9:\"BOSCHI, E\";i:11;s:10:\"CAPUANO, P\";i:12;s:12:\"DE FRANCO, R\";i:13;s:16:\"DELL'AVERSANA, P\";}s:9:\"\u0000*\u0000aucorp\";s:0:\"\";s:7:\"\u0000*\u0000isbn\";s:0:\"\";s:8:\"\u0000*\u0000coden\";s:6:\"SCIEAS\";s:8:\"\u0000*\u0000genre\";s:7:\"article\";s:7:\"\u0000*\u0000part\";s:0:\"\";s:9:\"\u0000*\u0000btitle\";s:0:\"\";s:8:\"\u0000*\u0000title\";s:82:\"Seismic evidence for a low-velocity zone in the upper crust beneath mount vesuvius\";s:8:\"\u0000*\u0000place\";s:14:\"Washington, DC\";s:6:\"\u0000*\u0000pub\";s:51:\"American Association for the Advancement of Science\";s:10:\"\u0000*\u0000edition\";s:0:\"\";s:9:\"\u0000*\u0000tpages\";s:0:\"\";s:9:\"\u0000*\u0000series\";s:0:\"\";s:8:\"\u0000*\u0000proxy\";s:30:\"http:\/\/proxyout.inist.fr:8080\/\";s:12:\"\u0000*\u0000integrite\";b:1;}"
Acceso mediante Panist
"O:12:\"IstexOpenUrl\":35:{s:10:\"\u0000*\u0000openUrl\";N;s:6:\"\u0000*\u0000fmt\";s:7:\"journal\";s:6:\"\u0000*\u0000doi\";s:0:\"\";s:6:\"\u0000*\u0000pii\";s:0:\"\";s:7:\"\u0000*\u0000pmid\";s:0:\"\";s:9:\"\u0000*\u0000atitle\";s:82:\"Seismic evidence for a low-velocity zone in the upper crust beneath mount vesuvius\";s:9:\"\u0000*\u0000jtitle\";s:26:\"Science (Washington, D.C.)\";s:9:\"\u0000*\u0000stitle\";s:20:\"Science (Wash. D.C.)\";s:7:\"\u0000*\u0000date\";s:4:\"1996\";s:9:\"\u0000*\u0000volume\";s:3:\"274\";s:8:\"\u0000*\u0000issue\";s:4:\"5287\";s:8:\"\u0000*\u0000spage\";s:3:\"592\";s:8:\"\u0000*\u0000epage\";s:3:\"594\";s:8:\"\u0000*\u0000pages\";s:0:\"\";s:7:\"\u0000*\u0000issn\";s:9:\"0036-8075\";s:8:\"\u0000*\u0000eissn\";s:0:\"\";s:9:\"\u0000*\u0000aulast\";s:5:\"ZOLLO\";s:10:\"\u0000*\u0000aufirst\";s:1:\"A\";s:9:\"\u0000*\u0000auinit\";s:0:\"\";s:10:\"\u0000*\u0000auinitm\";s:0:\"\";s:5:\"\u0000*\u0000au\";a:14:{i:0;s:12:\"GASPARINI, P\";i:1;s:13:\"DE MATTEIS, R\";i:2;s:9:\"GUERRA, I\";i:3;s:13:\"LANNACCONE, G\";i:4;s:11:\"MIRABILE, L\";i:5;s:10:\"VILARDO, G\";i:6;s:10:\"VIRIEUX, J\";i:7;s:10:\"LE MEUR, H\";i:8;s:12:\"DE NATALE, G\";i:9;s:9:\"BIELLA, G\";i:10;s:9:\"BOSCHI, E\";i:11;s:10:\"CAPUANO, P\";i:12;s:12:\"DE FRANCO, R\";i:13;s:16:\"DELL'AVERSANA, P\";}s:9:\"\u0000*\u0000aucorp\";s:0:\"\";s:7:\"\u0000*\u0000isbn\";s:0:\"\";s:8:\"\u0000*\u0000coden\";s:6:\"SCIEAS\";s:8:\"\u0000*\u0000genre\";s:7:\"article\";s:7:\"\u0000*\u0000part\";s:0:\"\";s:9:\"\u0000*\u0000btitle\";s:0:\"\";s:8:\"\u0000*\u0000title\";s:82:\"Seismic evidence for a low-velocity zone in the upper crust beneath mount vesuvius\";s:8:\"\u0000*\u0000place\";s:14:\"Washington, DC\";s:6:\"\u0000*\u0000pub\";s:51:\"American Association for the Advancement of Science\";s:10:\"\u0000*\u0000edition\";s:0:\"\";s:9:\"\u0000*\u0000tpages\";s:0:\"\";s:9:\"\u0000*\u0000series\";s:0:\"\";s:8:\"\u0000*\u0000proxy\";s:30:\"http:\/\/proxyout.inist.fr:8080\/\";s:12:\"\u0000*\u0000integrite\";b:1;}"
Acceso mediante Istex
"O:16:\"EuropePMCOpenUrl\":35:{s:10:\"\u0000*\u0000openUrl\";N;s:6:\"\u0000*\u0000fmt\";s:7:\"journal\";s:6:\"\u0000*\u0000doi\";s:0:\"\";s:6:\"\u0000*\u0000pii\";s:0:\"\";s:7:\"\u0000*\u0000pmid\";s:0:\"\";s:9:\"\u0000*\u0000atitle\";s:82:\"Seismic evidence for a low-velocity zone in the upper crust beneath mount vesuvius\";s:9:\"\u0000*\u0000jtitle\";s:26:\"Science (Washington, D.C.)\";s:9:\"\u0000*\u0000stitle\";s:20:\"Science (Wash. D.C.)\";s:7:\"\u0000*\u0000date\";s:4:\"1996\";s:9:\"\u0000*\u0000volume\";s:3:\"274\";s:8:\"\u0000*\u0000issue\";s:4:\"5287\";s:8:\"\u0000*\u0000spage\";s:3:\"592\";s:8:\"\u0000*\u0000epage\";s:3:\"594\";s:8:\"\u0000*\u0000pages\";s:0:\"\";s:7:\"\u0000*\u0000issn\";s:9:\"0036-8075\";s:8:\"\u0000*\u0000eissn\";s:0:\"\";s:9:\"\u0000*\u0000aulast\";s:5:\"ZOLLO\";s:10:\"\u0000*\u0000aufirst\";s:1:\"A\";s:9:\"\u0000*\u0000auinit\";s:0:\"\";s:10:\"\u0000*\u0000auinitm\";s:0:\"\";s:5:\"\u0000*\u0000au\";a:14:{i:0;s:12:\"GASPARINI, P\";i:1;s:13:\"DE MATTEIS, R\";i:2;s:9:\"GUERRA, I\";i:3;s:13:\"LANNACCONE, G\";i:4;s:11:\"MIRABILE, L\";i:5;s:10:\"VILARDO, G\";i:6;s:10:\"VIRIEUX, J\";i:7;s:10:\"LE MEUR, H\";i:8;s:12:\"DE NATALE, G\";i:9;s:9:\"BIELLA, G\";i:10;s:9:\"BOSCHI, E\";i:11;s:10:\"CAPUANO, P\";i:12;s:12:\"DE FRANCO, R\";i:13;s:16:\"DELL'AVERSANA, P\";}s:9:\"\u0000*\u0000aucorp\";s:0:\"\";s:7:\"\u0000*\u0000isbn\";s:0:\"\";s:8:\"\u0000*\u0000coden\";s:6:\"SCIEAS\";s:8:\"\u0000*\u0000genre\";s:7:\"article\";s:7:\"\u0000*\u0000part\";s:0:\"\";s:9:\"\u0000*\u0000btitle\";s:0:\"\";s:8:\"\u0000*\u0000title\";s:82:\"Seismic evidence for a low-velocity zone in the upper crust beneath mount vesuvius\";s:8:\"\u0000*\u0000place\";s:14:\"Washington, DC\";s:6:\"\u0000*\u0000pub\";s:51:\"American Association for the Advancement of Science\";s:10:\"\u0000*\u0000edition\";s:0:\"\";s:9:\"\u0000*\u0000tpages\";s:0:\"\";s:9:\"\u0000*\u0000series\";s:0:\"\";s:8:\"\u0000*\u0000proxy\";s:30:\"http:\/\/proxyout.inist.fr:8080\/\";s:12:\"\u0000*\u0000integrite\";b:1;}"
Acceso mediante Europe PubMed Central
"O:11:\"BaseOpenUrl\":35:{s:10:\"\u0000*\u0000openUrl\";N;s:6:\"\u0000*\u0000fmt\";s:7:\"journal\";s:6:\"\u0000*\u0000doi\";s:0:\"\";s:6:\"\u0000*\u0000pii\";s:0:\"\";s:7:\"\u0000*\u0000pmid\";s:0:\"\";s:9:\"\u0000*\u0000atitle\";s:82:\"Seismic evidence for a low-velocity zone in the upper crust beneath mount vesuvius\";s:9:\"\u0000*\u0000jtitle\";s:26:\"Science (Washington, D.C.)\";s:9:\"\u0000*\u0000stitle\";s:20:\"Science (Wash. D.C.)\";s:7:\"\u0000*\u0000date\";s:4:\"1996\";s:9:\"\u0000*\u0000volume\";s:3:\"274\";s:8:\"\u0000*\u0000issue\";s:4:\"5287\";s:8:\"\u0000*\u0000spage\";s:3:\"592\";s:8:\"\u0000*\u0000epage\";s:3:\"594\";s:8:\"\u0000*\u0000pages\";s:0:\"\";s:7:\"\u0000*\u0000issn\";s:9:\"0036-8075\";s:8:\"\u0000*\u0000eissn\";s:0:\"\";s:9:\"\u0000*\u0000aulast\";s:5:\"ZOLLO\";s:10:\"\u0000*\u0000aufirst\";s:1:\"A\";s:9:\"\u0000*\u0000auinit\";s:0:\"\";s:10:\"\u0000*\u0000auinitm\";s:0:\"\";s:5:\"\u0000*\u0000au\";a:14:{i:0;s:12:\"GASPARINI, P\";i:1;s:13:\"DE MATTEIS, R\";i:2;s:9:\"GUERRA, I\";i:3;s:13:\"LANNACCONE, G\";i:4;s:11:\"MIRABILE, L\";i:5;s:10:\"VILARDO, G\";i:6;s:10:\"VIRIEUX, J\";i:7;s:10:\"LE MEUR, H\";i:8;s:12:\"DE NATALE, G\";i:9;s:9:\"BIELLA, G\";i:10;s:9:\"BOSCHI, E\";i:11;s:10:\"CAPUANO, P\";i:12;s:12:\"DE FRANCO, R\";i:13;s:16:\"DELL'AVERSANA, P\";}s:9:\"\u0000*\u0000aucorp\";s:0:\"\";s:7:\"\u0000*\u0000isbn\";s:0:\"\";s:8:\"\u0000*\u0000coden\";s:6:\"SCIEAS\";s:8:\"\u0000*\u0000genre\";s:7:\"article\";s:7:\"\u0000*\u0000part\";s:0:\"\";s:9:\"\u0000*\u0000btitle\";s:0:\"\";s:8:\"\u0000*\u0000title\";s:82:\"Seismic evidence for a low-velocity zone in the upper crust beneath mount vesuvius\";s:8:\"\u0000*\u0000place\";s:14:\"Washington, DC\";s:6:\"\u0000*\u0000pub\";s:51:\"American Association for the Advancement of Science\";s:10:\"\u0000*\u0000edition\";s:0:\"\";s:9:\"\u0000*\u0000tpages\";s:0:\"\";s:9:\"\u0000*\u0000series\";s:0:\"\";s:8:\"\u0000*\u0000proxy\";s:30:\"http:\/\/proxyout.inist.fr:8080\/\";s:12:\"\u0000*\u0000integrite\";b:1;}"
Acceso mediante Base Search
"O:12:\"ArXivOpenUrl\":35:{s:10:\"\u0000*\u0000openUrl\";N;s:6:\"\u0000*\u0000fmt\";s:7:\"journal\";s:6:\"\u0000*\u0000doi\";s:0:\"\";s:6:\"\u0000*\u0000pii\";s:0:\"\";s:7:\"\u0000*\u0000pmid\";s:0:\"\";s:9:\"\u0000*\u0000atitle\";s:82:\"Seismic evidence for a low-velocity zone in the upper crust beneath mount vesuvius\";s:9:\"\u0000*\u0000jtitle\";s:26:\"Science (Washington, D.C.)\";s:9:\"\u0000*\u0000stitle\";s:20:\"Science (Wash. D.C.)\";s:7:\"\u0000*\u0000date\";s:4:\"1996\";s:9:\"\u0000*\u0000volume\";s:3:\"274\";s:8:\"\u0000*\u0000issue\";s:4:\"5287\";s:8:\"\u0000*\u0000spage\";s:3:\"592\";s:8:\"\u0000*\u0000epage\";s:3:\"594\";s:8:\"\u0000*\u0000pages\";s:0:\"\";s:7:\"\u0000*\u0000issn\";s:9:\"0036-8075\";s:8:\"\u0000*\u0000eissn\";s:0:\"\";s:9:\"\u0000*\u0000aulast\";s:5:\"ZOLLO\";s:10:\"\u0000*\u0000aufirst\";s:1:\"A\";s:9:\"\u0000*\u0000auinit\";s:0:\"\";s:10:\"\u0000*\u0000auinitm\";s:0:\"\";s:5:\"\u0000*\u0000au\";a:14:{i:0;s:12:\"GASPARINI, P\";i:1;s:13:\"DE MATTEIS, R\";i:2;s:9:\"GUERRA, I\";i:3;s:13:\"LANNACCONE, G\";i:4;s:11:\"MIRABILE, L\";i:5;s:10:\"VILARDO, G\";i:6;s:10:\"VIRIEUX, J\";i:7;s:10:\"LE MEUR, H\";i:8;s:12:\"DE NATALE, G\";i:9;s:9:\"BIELLA, G\";i:10;s:9:\"BOSCHI, E\";i:11;s:10:\"CAPUANO, P\";i:12;s:12:\"DE FRANCO, R\";i:13;s:16:\"DELL'AVERSANA, P\";}s:9:\"\u0000*\u0000aucorp\";s:0:\"\";s:7:\"\u0000*\u0000isbn\";s:0:\"\";s:8:\"\u0000*\u0000coden\";s:6:\"SCIEAS\";s:8:\"\u0000*\u0000genre\";s:7:\"article\";s:7:\"\u0000*\u0000part\";s:0:\"\";s:9:\"\u0000*\u0000btitle\";s:0:\"\";s:8:\"\u0000*\u0000title\";s:82:\"Seismic evidence for a low-velocity zone in the upper crust beneath mount vesuvius\";s:8:\"\u0000*\u0000place\";s:14:\"Washington, DC\";s:6:\"\u0000*\u0000pub\";s:51:\"American Association for the Advancement of Science\";s:10:\"\u0000*\u0000edition\";s:0:\"\";s:9:\"\u0000*\u0000tpages\";s:0:\"\";s:9:\"\u0000*\u0000series\";s:0:\"\";s:8:\"\u0000*\u0000proxy\";s:30:\"http:\/\/proxyout.inist.fr:8080\/\";s:12:\"\u0000*\u0000integrite\";b:1;}"
Acceso mediante arXiv
