Zobrazeno 1 - 10
of 38
pro vyhledávání: '"Vittorio Scisciani"'
Publikováno v:
Scientific Reports, Vol 13, Iss 1, Pp 1-17 (2023)
Abstract Two slightly lithified volcanic rich layers (VRL) (former tephra) SVT-2 (San Vittorino) and CAC (Castiglione a Casauria) were sampled from two distinct post-evaporitic Messinian stratigraphic sections (Abruzzo, Central Italy). They crop only
Externí odkaz:
https://doaj.org/article/cfefd41bd38c4458a3539d23cfdc5bdc
Autor:
Davide Potere, Vittorio Scisciani, Monica Piochi, Pietro Paolo Pierantoni, Angela Mormone, Manuela Nazzari, Piergiorgio Scarlato, Gianluca Iezzi
Publikováno v:
Minerals, Vol 12, Iss 7, p 893 (2022)
A Messinian and lithified horizon enriched in volcanic particles with thicknesses of 170–180 cm crops in the Camporotondo (CR) section (Marche, Italy). This volcanic-rich layer (VRL) was investigated by field plus mesoscopic observations, X-ray pow
Externí odkaz:
https://doaj.org/article/cedeea4439a34c789ecbe61619ec8090
Autor:
Alberto Pizzi, Vittorio Scisciani
Publikováno v:
Annals of Geophysics, Vol 55, Iss 4 (2012)
On May 20, 2012, a Ml 5.9 earthquake (T1) occurred in the Emilia-Romagna Region of northern Italy. This was preceded by a Ml 4.1 foreshock on May 19, 2012, and followed by several aftershocks, including two Ml 5.1 events, both on the same day. On May
Externí odkaz:
https://doaj.org/article/9abb3f6da3834eb7a8877f4bac418f9d
Modelling of potential fields can significantly contribute to the understanding of the subsurface geology, particularly if constrained by field geology, well-data and seismic profiles. This approach becomes crucial to define the subsurface setting wh
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d5d9b56108b4f81d5ba0335eb8466bd9
https://doi.org/10.5194/egusphere-egu23-684
https://doi.org/10.5194/egusphere-egu23-684
Publikováno v:
Geological Society, London, Special Publications. 494:301-331
Well penetrations on the UK East Shetland Platform (ESP) prove 1–8 km-thick Devonian post-orogenic extensional collapse-related successions. Conversely, extremely thick (1–6 km) Permo-Triassic basin-fills without Devono-Carboniferous units were i
Autor:
Stefano Patruno, Vittorio Scisciani
Publikováno v:
Basin Research. 33:2118-2156
[Abstract Normal faults grow either by radial propagation and segment linkage or by accruing displacement without a proportional increase in fault length. To test these competing models of fault growth, a novel 2D seismic stratigraphic interpretation
Autor:
Claudio Pellegrini, Vittorio Scisciani, Stefano Patruno, William Helland-Hansen, Nico D'Intino, William Reid
Publikováno v:
Basin research
32 (2020): 224–239. doi:10.1111/bre.12379
info:cnr-pdr/source/autori:Patruno, Stefano; Scisciani, Vittorio; Helland-Hansen, William; D'Intino, Nico; Reid, William; Pellegrini, Claudio/titolo:Upslope-climbing shelf-edge clinoforms and the stepwise evolution of the northern European glaciation (lower Pleistocene Eridanos Delta system, UK North Sea): When sediment supply overwhelms accommodation/doi:10.1111%2Fbre.12379/rivista:Basin research (Print)/anno:2020/pagina_da:224/pagina_a:239/intervallo_pagine:224–239/volume:32
32 (2020): 224–239. doi:10.1111/bre.12379
info:cnr-pdr/source/autori:Patruno, Stefano; Scisciani, Vittorio; Helland-Hansen, William; D'Intino, Nico; Reid, William; Pellegrini, Claudio/titolo:Upslope-climbing shelf-edge clinoforms and the stepwise evolution of the northern European glaciation (lower Pleistocene Eridanos Delta system, UK North Sea): When sediment supply overwhelms accommodation/doi:10.1111%2Fbre.12379/rivista:Basin research (Print)/anno:2020/pagina_da:224/pagina_a:239/intervallo_pagine:224–239/volume:32
[Abstract Clinoforms are basinward‐dipping and accreting palaeo‐bathymetric profiles that record palaeo‐environmental conditions and processes; thus, clinothems represent natural palaeo‐archives. Here, we document shelf‐edge scale clinoform
Autor:
Vittorio Scisciani, Fernando Calamita, Stefano Patruno, Enrico Tavarnelli, David Iacopini, Paolo Pace
Publikováno v:
Geological Society, London, Special Publications. 470:205-243
The core of the island of Cyprus hosts the inverted Troodos ophiolitic zone, whose flanks are overlain by autochthonous sedimentary rocks, mostly comprising Cenozoic-age carbonate shelf units. Some of these units are likely analogous to the Miocene p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::67b7c3e5b046f842d249d432008fe5a3
https://doi.org/10.5194/egusphere-egu21-6485
https://doi.org/10.5194/egusphere-egu21-6485