1,721,209 research outputs found
Geometrie delle deformazioni della Sabina meridionale attraverso la ricostruzione di superfici strutturali (Lazio, Appennino centrale)
No full textItinerario n.5. Da Palestrina ad Alatri attraverso i Monti Prenestini ed Ernici (km 183). Dalla scarpata alla laguna interna attraverso la soglia della Piattaforma carbonatica laziale-abruzzese; i rapporti con l’avanfossa tortoniana; stili deformativi a confronto a E e a W della linea Olevano-Antrodoco
No full textItinerario N° 8 - Valle del Turano, valle del Salto, alta valle del Velino. Le falde sabine, l’avanfossa messiniana e la linea tettonica Olévano-Antrodoco; le successioni Sabine e la “soglia” del M. Nùria.
No full textItinerario N° 6 – Da Settecamini a Settebagni, attraverso i Monti Lucrètili. la successione meso-cenozoica in facies di transizione e la struttura a falde della Sabina. La storia geologica della Campagna Romana.
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Assetto strutturale dei Monti Lucretili settentrionali (Sabina): nuovi dati e schema tettonico preliminare
No full textNeogene compressive deformations of the Latina Valley thrust front hangingwall: kinematics and geometry of the Montelanico-Carpineto backthrust (Central Italy)
No full textGeometry and kinematics of the Montelanico-Carpineto Backthrust (Lepini Mts., Latium) in the hangingwall of the early Messinian thrust front of the central Apennines: implications for the Apennine chain building
No full textStructural geological sections taken from the railway tunnel through the Monte Bove and Saint Mary hills, Aquila-Abruzzi
No full textThe stratigraphic and structural data obtained from the study carried out on the samples collected inside the Monte Bove railway tunnel (Carseolani Mts., Abruzzo), allowed a reconstruction of the complicated tectonics of the surrounding area. The sequence recovered inside the tunnel is wholly calcareous and was dated as Late Cretaceous and Middle Miocene. The lithologies are described. The western part of the geologic section is formed by small fragments of monoclines (constituted by Miocene and Cretaceous limestones), affected by subvertical extensional tectonics. The central part is characterized by two ramp-flat structures, which develop on the ductile layer of the "Marne a Orbulina' and generate the overthrust of the Cretaceous limestones on the whole Miocene sequence. The eastern part comprises several fragments of the succession, doubled and repeated by ridge structures associated with a transcurrent phase. -from English summar
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