Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Federico, Mantovani"'
Autor:
Franco Marco Elter, Federico Mantovani
Publikováno v:
Geosciences, Vol 14, Iss 10, p 260 (2024)
This study presents an updated interpretation of geological data collected between 1984 and 2022. The area under consideration holds significant regional importance as it is located between the Internal Nappe Zone (INZ) and the Regional Mylonitic Com
Externí odkaz:
https://doaj.org/article/40af709e221845b8aadf21fa34ae127f
Autor:
Federico Mantovani, Franco Marco Elter
Publikováno v:
Geosciences, Vol 14, Iss 5, p 113 (2024)
Sardinia (Italy) represents one of the most comprehensive cross-sections of the Variscan orogen. The metamorphic and structural complexity characterizing its axial zone still presents many unresolved issues in the current state of knowledge. The data
Externí odkaz:
https://doaj.org/article/d0b49f582c0446e29fd415183748093a
Publikováno v:
Geosciences, Vol 13, Iss 6, p 154 (2023)
The Portofino Conglomerate (PC) cropping out in the Eastern Liguria is an approximately 500 m thick, very gently folded succession mainly composed of poorly bedded and mostly matrix-supported conglomerates. It stratigraphically rests on the Helmintho
Externí odkaz:
https://doaj.org/article/1c4228280b8a4535914d2c1344572895
Autor:
Laura Gaggero, Federico Mantovani, Franco Marco Elter, Luca Giacomo Costamagna, Enrico Pandeli
Publikováno v:
International journal of earth sciences (1999, Internet) 109 (2020): 739–760. doi:10.1007/s00531-020-01830-y
info:cnr-pdr/source/autori:Elter F.M.[1], Gaggero L.[1], Mantovani F.[1], Pandeli E.[2,3], Costamagna L.G.[4]/titolo:The Atlas-East Variscan-Elbe shear system and its role in the formation of the pull-apart Late Palaeozoic basins/doi:10.1007%2Fs00531-020-01830-y/rivista:International journal of earth sciences (1999, Internet)/anno:2020/pagina_da:739/pagina_a:760/intervallo_pagine:739–760/volume:109
info:cnr-pdr/source/autori:Elter F.M.[1], Gaggero L.[1], Mantovani F.[1], Pandeli E.[2,3], Costamagna L.G.[4]/titolo:The Atlas-East Variscan-Elbe shear system and its role in the formation of the pull-apart Late Palaeozoic basins/doi:10.1007%2Fs00531-020-01830-y/rivista:International journal of earth sciences (1999, Internet)/anno:2020/pagina_da:739/pagina_a:760/intervallo_pagine:739–760/volume:109
The Variscan orogeny occurred as a result of the Late Devonian to Late Carboniferous collision and accretion of Gondwana-derived microcontinents and continental masses with those of Laurussia. The irregular boundaries of the colliding continents caus
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::402aa0fac243d2398ebae3577d96edfc
https://publications.cnr.it/doc/458941
https://publications.cnr.it/doc/458941
Publikováno v:
Minerals
Volume 9
Issue 9
Minerals, Vol 9, Iss 9, p 539 (2019)
Volume 9
Issue 9
Minerals, Vol 9, Iss 9, p 539 (2019)
The aim of this work was to establish whether asbestos fibers homogeneously occur in the different fractions ground from naturally occurring asbestos lithotypes, and to calculate the contribution of fibers from each fraction to the overall concentrat
In the early Cambrian Bithia Formation in the Variscan foreland of Sardinia, a Middle Ordovician granitic intrusion (478–457 Ma) is hosted by marly metasedimentary rocks that were affected by high-temperature (HT) metamorphism. A detailed structura
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1e1e6c54798c55742b5a3413c26b6c97
http://hdl.handle.net/11567/851541
http://hdl.handle.net/11567/851541
Publikováno v:
The Review of scientific instruments. 82(12)
A flow monitoring system based on a constant temperature hot-film anemometer is presented. The device has been designed to monitor a dispensing process of extremely low quantities of adhesive material. The monitoring device presented in this paper is