http://www.cnr.it/ontology/cnr/individuo/prodotto/ID201386
Middle-late jurassic syndepositional tectonics recorded in the ligurian Briançonnais succession (Marguareis-Mongioie area, Ligurian Alps, NW Italy) (Articolo in rivista)
- Type
- Label
- Middle-late jurassic syndepositional tectonics recorded in the ligurian Briançonnais succession (Marguareis-Mongioie area, Ligurian Alps, NW Italy) (Articolo in rivista) (literal)
- Anno
- 2011-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1007/s00015-011-0058-0 (literal)
- Alternative label
Bertok, C. [ 1 ] ; Martire, L. [ 1 ] ; Perotti, E. [ 1 ] ; d'Atri, A. [ 1 ] ; Piana, F. [ 2 ] (2011)
Middle-late jurassic syndepositional tectonics recorded in the ligurian Briançonnais succession (Marguareis-Mongioie area, Ligurian Alps, NW Italy)
in Swiss journal of geosciences (Print)
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Bertok, C. [ 1 ] ; Martire, L. [ 1 ] ; Perotti, E. [ 1 ] ; d'Atri, A. [ 1 ] ; Piana, F. [ 2 ] (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#altreInformazioni
- ID_PUMA : cnr.igg/2011-A0-088 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- [ 1 ] Univ Turin, Dept Earth Sci, I-10125 Turin, Italy
[ 2 ] CNR, Inst Geosci & Earth Resources, Turin Unit, I-10125 Turin, Italy (literal)
- Titolo
- Middle-late jurassic syndepositional tectonics recorded in the ligurian Briançonnais succession (Marguareis-Mongioie area, Ligurian Alps, NW Italy) (literal)
- Abstract
- The Middle-Upper Jurassic succession of the Marguareis-Mongioie area (Ligurian Brianconnais Domain), developed in a protected shelf environment evolving into a pelagic plateau, bears clear evidence of synsedimentary tectonics such as: growth fault-related structures; neptunian dykes; marked lateral variations in stratigraphic thicknesses testifying to the juxtaposition of sectors characterized by different sedimentation and subsidence rates; discordant, anomalous stratigraphic contacts corresponding to paleoescarpments; nodular beds showing evidence of fluidification interpreted as seismites; and the occurrence of sand-sized quartz grains pointing to denudation of Permo-Triassic quartz-rich rocks. Such evidence documents an important Middle-Late Jurassic post-breakup tectonic activity, which was more effective in controlling the basin topography than the Early Jurassic syn-rift tectonic phase. Two main tectono-sedimentary stages, one occurring during the Bathonian, the other falling within the Callovian-Kimmeridgian interval, were reconstructed. The first stage can be referred to a fault-related activity occurring shortly after the initial stages of oceanic spreading of the Ligurian Tethys; the second can be genetically related to the far effects of the first rifting stage of the Bay of Biscay and the Valais basin. (literal)
- Prodotto di
- Autore CNR
- Insieme di parole chiave
Incoming links:
- Autore CNR di
- Prodotto
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#rivistaDi
- Insieme di parole chiave di