Zobrazeno 1 - 10
of 14
pro vyhledávání: '"SANDRO VENTURINI"'
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 92, Iss 3 (2020)
he aim of this work is the stratigraphic revision of the sequences outcropping on the southwestern side of the M. Mia — M. Matajur anticline. This area, until now, was poorly studied from a geological point of view. Norian to Lower Cuisian strata w
Externí odkaz:
https://doaj.org/article/c59b4d7ebc8445ea99b472f2040bef13
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 93, Iss 2 (2020)
This paper deals with the stratigraphy of well SPAN 1 (San Pietro al Natisone, Eastern Friuli). The stratigraphic sequence is composed by Paleocenic flysch deposits (from 69 m to 748 m), Maastrichtian resedimented carbonates (from 748 m to 940 m) and
Externí odkaz:
https://doaj.org/article/ab9cbe3b699f496dab33f7d3cd60afb7
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 101, Iss 1 (2017)
A tridactyl footprint referable to a theropod dinosaur, found on a limestone block of Late Hauterivian age, is described here. The block was used to build the pier of Porto Corsini (Ravenna, Italy); the site of provenance is located on the southern f
Externí odkaz:
https://doaj.org/article/597da23b2b9044b889a73e60f728ce70
Publikováno v:
Geologia Croatica, Vol 45, Iss 0, Pp 87-93 (2010)
The Early Middle Cenomanian margin sequence of Val ludrio, connected with the northeastem margin of the Friuli Platform shows intercalated layers with pelagic organisms: Calcisphaerulidae and planktonic forams, among which is Favwsella. These are int
Externí odkaz:
https://doaj.org/article/5d2190729cb54e628648a74c8c21c5bc
Autor:
Giorgio Tunis, Sandro Venturini
Publikováno v:
Geologia Croatica, Vol 45, Iss 0, Pp 127-150 (2010)
From the Maaslrichtian up to the Early Eocene, the Julian (or Slovenian) Basin is characterized by a mixed siliciclastic/carbonale deposits system which exhibit complex sedimentalion patterns depending on various controls: sea level changes; tectonic
Externí odkaz:
https://doaj.org/article/67468db86b68489ab872f48f838c49e1
Autor:
Fabrizio, Bizzarini, Paolo, Maddaleni, Giuseppe, Muscio, Ponton, Maurizio, Luca, Simonetto, Sandro, Venturini
Isolated reliefs crops out in the upper Friulian Plain (Friuli Venezia Giulia Autonomous Region, NE Italy). The north-western portion of one of them, near Pozzuolo del Friuli, is made of Miocene sandstone. Geology and fossils collected in that sandst
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::1cd8bf31fe3a5c505cdfa5271d5f41cf
https://hdl.handle.net/11368/2980560
https://hdl.handle.net/11368/2980560
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 140:245-269
During the Early Cretaceous, wide areas of the Dinaric–Adriatic Carbonate Platform emerged for long periods. The Hauterivian–Barremian carbonates from Kolone–Barbariga show a few typical examples of lacustrine facies with dinosaur bones and bra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f3a024a7a8e3f30812ddb5df6f8c7c7d
https://doi.org/10.1016/s0031-0182(98)00042-x
https://doi.org/10.1016/s0031-0182(98)00042-x
Autor:
Francesco Italiano, Davide Baldini, Stefano Mazzoni, Carmelo Baio, Stefano Cantini, Daniele Loi, Sandro Venturini, Massimiliano Borghi
Publikováno v:
All Days.
Several offshore gas fields are present in Adriatic Sea (Italy), producing since the 60s from multilayer metric sand reservoirs. The declining production in these mature fields is normally offset by drilling new deviated wells. Recent technology evol
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::81a3f899ff7922778d4bc2146e6f172c
https://doi.org/10.2118/154426-ms
https://doi.org/10.2118/154426-ms
In central Istria (western Croatia) a middle Eocene unit, some tens of metres thick, marks the transition from shallow-water carbonate to deeper-water clastic sedimentation. This unit consists of a basal interval, rich in macrofossils, made of clayey
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3189f827e70bde677e0145c4d38c478c
http://hdl.handle.net/11368/1701952
http://hdl.handle.net/11368/1701952