IL SOVRASCORRIMENTO DELL'UNITA' TRASIMENO SULLA SUCCESSIONE UMBRA DELLA ZONA DI UMBERTIDE: DATI STRATIGRAFICI E STRUTTURALI
A sector of the Umbrian thrust belt is examined here: the '' Argille vari colori line'' near Umbertide (Tevere Valley) in which the Trasimeno Unit thrusts over the Umbrian succession. From a biostratigraphic point of view the uppermost part of the Umbrian succession (i.e. the Ma...
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Università di Camerino
1992
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ftdatacite:10.15165/studgeocam-792 2023-05-15T18:00:47+02:00 IL SOVRASCORRIMENTO DELL'UNITA' TRASIMENO SULLA SUCCESSIONE UMBRA DELLA ZONA DI UMBERTIDE: DATI STRATIGRAFICI E STRUTTURALI CERRINA FERONI, A. PLESI, G. PRIAMI, F. 1992 https://dx.doi.org/10.15165/studgeocam-792 http://193.204.8.201:8080/jspui/handle/1336/137 unknown Università di Camerino Geologia strutturale - Biostratigrafia - Thrusts - Appennino settentrionale Structural Geology - Biostratigraphy - Thrusts - Northern Apennines CreativeWork article 1992 ftdatacite https://doi.org/10.15165/studgeocam-792 2021-11-05T12:55:41Z A sector of the Umbrian thrust belt is examined here: the '' Argille vari colori line'' near Umbertide (Tevere Valley) in which the Trasimeno Unit thrusts over the Umbrian succession. From a biostratigraphic point of view the uppermost part of the Umbrian succession (i.e. the Marnoso-arenacea formation) and the Trasimeno succession were analyzed. The Marnoso-arenacea formation belongs, on the basis of its planktonic foraminifera contents, to the N7 Bww biozone. The top of the formation corresponds to the uppermost part of the same biozone. The Argille varicolori formati on of the Tuscan succession belongs to the N3 Bww biozone and it is entirely comprised in the Oligocene. The Trasimeno Miogypsina sandstone basal levels were also re-examined. They result early-Aquitanian in age on the basis of the study of Miogypsina embryonic apparatus evolution degree. [...] Article in Journal/Newspaper Planktonic foraminifera DataCite Metadata Store (German National Library of Science and Technology) |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
topic |
Geologia strutturale - Biostratigrafia - Thrusts - Appennino settentrionale Structural Geology - Biostratigraphy - Thrusts - Northern Apennines |
spellingShingle |
Geologia strutturale - Biostratigrafia - Thrusts - Appennino settentrionale Structural Geology - Biostratigraphy - Thrusts - Northern Apennines CERRINA FERONI, A. PLESI, G. PRIAMI, F. IL SOVRASCORRIMENTO DELL'UNITA' TRASIMENO SULLA SUCCESSIONE UMBRA DELLA ZONA DI UMBERTIDE: DATI STRATIGRAFICI E STRUTTURALI |
topic_facet |
Geologia strutturale - Biostratigrafia - Thrusts - Appennino settentrionale Structural Geology - Biostratigraphy - Thrusts - Northern Apennines |
description |
A sector of the Umbrian thrust belt is examined here: the '' Argille vari colori line'' near Umbertide (Tevere Valley) in which the Trasimeno Unit thrusts over the Umbrian succession. From a biostratigraphic point of view the uppermost part of the Umbrian succession (i.e. the Marnoso-arenacea formation) and the Trasimeno succession were analyzed. The Marnoso-arenacea formation belongs, on the basis of its planktonic foraminifera contents, to the N7 Bww biozone. The top of the formation corresponds to the uppermost part of the same biozone. The Argille varicolori formati on of the Tuscan succession belongs to the N3 Bww biozone and it is entirely comprised in the Oligocene. The Trasimeno Miogypsina sandstone basal levels were also re-examined. They result early-Aquitanian in age on the basis of the study of Miogypsina embryonic apparatus evolution degree. [...] |
format |
Article in Journal/Newspaper |
author |
CERRINA FERONI, A. PLESI, G. PRIAMI, F. |
author_facet |
CERRINA FERONI, A. PLESI, G. PRIAMI, F. |
author_sort |
CERRINA FERONI, A. |
title |
IL SOVRASCORRIMENTO DELL'UNITA' TRASIMENO SULLA SUCCESSIONE UMBRA DELLA ZONA DI UMBERTIDE: DATI STRATIGRAFICI E STRUTTURALI |
title_short |
IL SOVRASCORRIMENTO DELL'UNITA' TRASIMENO SULLA SUCCESSIONE UMBRA DELLA ZONA DI UMBERTIDE: DATI STRATIGRAFICI E STRUTTURALI |
title_full |
IL SOVRASCORRIMENTO DELL'UNITA' TRASIMENO SULLA SUCCESSIONE UMBRA DELLA ZONA DI UMBERTIDE: DATI STRATIGRAFICI E STRUTTURALI |
title_fullStr |
IL SOVRASCORRIMENTO DELL'UNITA' TRASIMENO SULLA SUCCESSIONE UMBRA DELLA ZONA DI UMBERTIDE: DATI STRATIGRAFICI E STRUTTURALI |
title_full_unstemmed |
IL SOVRASCORRIMENTO DELL'UNITA' TRASIMENO SULLA SUCCESSIONE UMBRA DELLA ZONA DI UMBERTIDE: DATI STRATIGRAFICI E STRUTTURALI |
title_sort |
il sovrascorrimento dell'unita' trasimeno sulla successione umbra della zona di umbertide: dati stratigrafici e strutturali |
publisher |
Università di Camerino |
publishDate |
1992 |
url |
https://dx.doi.org/10.15165/studgeocam-792 http://193.204.8.201:8080/jspui/handle/1336/137 |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_doi |
https://doi.org/10.15165/studgeocam-792 |
_version_ |
1766170019075457024 |