Subsurface statigraphy of Middle Pleistocene continental deposits from Livorno area and biostratigraphic characterization of the Pleistocene

Autor: Ciampalini A.[1], Da Prato S.[2], Catanzariti R.[2], Colonese A.[3], Michelucci L.[4], Zanchetta G. [1]

Publikováno v: Atti della Società toscana di scienze naturali residente in Pisa. Memorie 120 (2013): 39–53. doi:10.2424/ASTSN.M.2013.12
info:cnr-pdr/source/autori:Ciampalini A.[1], Da Prato S.[2], Catanzariti R.[2], Colonese A.[3], Michelucci L.[4], Zanchetta G. [1]/titolo:Subsurface statigraphy of Middle Pleistocene continental deposits from Livorno area and biostratigraphic characterization of the Pleistocene.../doi:10.2424%2FASTSN.M.2013.12/rivista:Atti della Società toscana di scienze naturali residente in Pisa. Memorie/anno:2013/pagina_da:39/pagina_a:53/intervallo_pagine:39–53/volume:120

The main results of an integrated study of 4 boreholes drilled in the subsurface of Livorno (NW Italy) are reported. Stratigraphic interpretations of the cores allowed the identification of 4 main lithostratigraphic units, that were correlated with u

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::5b60760fd74189e25697fff38393121e

Interactions between tectonic and sedimentation related to the Rides Prérifaines in the Volubilis basin (Rif front, Morocco)

Autor: Roldán García, F. J., Galindo Zaldívar, Jesús, Chalouan, Ahmed, Anahnah, Farida, Ahmamou, M., Ruano, P., Constán, Ana Ruiz, Sanz de Galdeano, Carlos, Benmakhlouf, M., Marín-Lechado, C., López-Garrido, A. C., Pedrera Parias, Antonio

Publikováno v: Digital.CSIC. Repositorio Institucional del CSIC
instname
Arias Montano. Repositorio Institucional de la Universidad de Huelva

4 páginas, 4 figuras.-- Trabajo presentado en la 47ª Sesión Científica, Santander, 2009.
The Volubilis Neogene basin (Morocco) was part of the South Rif Corridor that connected the Atlantic Ocean with the Mediterranean. This basin recorded t

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::0ab0d9212f33c1bf5c0d9ec2b68af1ed
http://hdl.handle.net/10261/29449

The age of the Paludi Formation: a major constraint to the beginning of the Apulia verging orogenic transport in the northern sector of the Calabria – Peloritani Arc

Autor: BONARDI, GLAUCO, DE CAPOA, PAOLA, DI STASO, ANGELIDA, PERRONE V., SONNINO M., TRAMONTANA M.

A stratigraphic revision of the Paludi Formation, cropping out in Northern Calabria on the north-eastern side of Sila Massif, has confirmed that it has been deposited between two main tectonic phases. Actually the formation is involved only by top to

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::1c030b9948e871fa1a37077b17f89264
http://hdl.handle.net/11588/350971

Palaeogeography of the late aquitanian-early Burdigalian basin in the western Betic Internal Zone

Autor: Francisco Serrano, Carlos Sanz de Galdeano, José Antonio Martín Pérez, Ángel Carlos López Garrido

Publikováno v: Digital.CSIC. Repositorio Institucional del CSIC
instname

13 páginas, 7 figuras, 1 tabla.
[EN] The discovery of new outcrops of transgressive sediments in the western Betic Internal Zone belonging to the UpperAquitanian-Lower Burdigalian (Blow's N.4?, N.5 and N.6 zones of planktonic foraminifera and C

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::79ca756c6ca281740706de9b96540249
http://hdl.handle.net/10261/31446

B. - Évolution d'après les critères micropaléontologiques

Autor: Carla Müller, Annik Brun, R. Desprat, Laure Blanc-Vernet, Marie Morzadec-Kerfourn, R.S.M. Templeton

Publikováno v: Géologie Méditerranéenne. 6:290-296

Micropaleontological studies of late-Quaternary sediments show the importance of the 27 000 B.P. transgression which is almost up to the actual shoreline and also of the 1 7 000 regression. The Versilian transgression moves from East to West on the G

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7e74c780b0758348374ebc14df298e04
https://doi.org/10.3406/geolm.1979.1091