Sicilia orientale. Profilo geologico Nebrodi-Iblei
- Autre titre
- La Sicile orientale. Coupe géologique Nebrodi-Iblei (fr)
- Auteur
- BIANCHI, F; CARBONE, S; GRASSO, M; INVERNIZZI, G; LENTINI, F; LONGARETTI, G; MERLINI, S; MOSTARDINI, F
AGIP spA, Milano, Italy - Nom de la conférence
- Convegno su : Sistemi avanfossa-avampaese lungo la Catena Appenninico-Maghrebide (1987-04-22)
- Source
Memorie della Societa Geologica Italiana. 1987, Vol 38, pp 429-458, 30 p ; Geological sketch map , Illustration , Section , Stratigraphic column ; ref : 2 p
- Editeur
- Societa geologica italiana, Roma
- Pays de publication
- Italy
- Type de document
- Conference Paper
- Langue
- Italian
- Mot clé (fr)
- Age Coupe géologique Couverture sédimentaire Ecaille tectonique Faille chevauchement Levé gravimétrique Levé sismique Lithofaciès Monts Nebrodi Notice explicative Puits reconnaissance Sicile Unité tectonique Europe Italie
- Mot clé (en)
- Age Sections Geological section Sedimentary cover Tectonic wedges Overthrust faults Gravity surveys Gravity survey Seismic surveys Lithofacies Nebrodi Mountains Explanatory text Wells Sicily Tectonic units Tectonic unit Europe Italy
- Mot clé (es)
- Edad Corte geológico Cubierta sedimentaria Cabalgamiento Levantamiento gravimétrico Levantamiento sísmico Litofácies Montes Nebrodi Nota explicativa Pozo de reconocimiento Sicilia Unidad tectónica Europa Italia
- Classification
- Pascal
- 001 Sciences exactes et technologie / 001E Terre, ocean, espace / 001E01 Sciences de la terre / 001E01J Géologie régionale. Cartes / 001E01J01 Géologie régionale
- Discipline
- Earth sciences
- Provenance
- BRGM
- Base de données
- PASCAL
- Identifiant INIST
- 19733732
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
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