Zobrazeno 1 - 10
of 202
pro vyhledávání: '"Alpine tectonics"'
Autor:
Francis Huguet
Publikováno v:
International Journal of Geoheritage and Parks, Vol 11, Iss 4, Pp 624-633 (2023)
The Matterhorn, a famous mountain in the Swiss Alps is a well characterized geomorphosite, presenting both an important scientific interest and aesthetic, cultural and economic values in Switzerland. The main scientific issues concerning the Matterho
Externí odkaz:
https://doaj.org/article/6517a6bef4aa4a4b92d6841a7313945e
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Autor:
Nemesio Heredia, Fidel Martín-González, Pedro Farias, Joaquín García-Sansegundo, David Pedreira, Brais Gonzalo-Guerra, Gabriel García-Davia, Guillermo Mateos, Adriana G. Flórez-Rodríguez
Publikováno v:
Journal of Maps, Vol 0, Iss 0, Pp 1-10 (2021)
The Cabuérniga Fault System (CFS) extends for 150 km in E–W trend along the northern divide of the Cantabrian Mountains, near the Cantabrian Sea. This fault system was reactivated several times since the Paleozoic, and displays hydrothermal activi
Externí odkaz:
https://doaj.org/article/dac6071dc68e473c9699b6af0d609022
Autor:
Gianni Balestro, Francesco Nosenzo, Paola Cadoppi, Gianfranco Fioraso, Chiara Groppo, Andrea Festa
Publikováno v:
Journal of Maps, Vol 16, Iss 2, Pp 736-744 (2020)
In the Valmala sector of the southern Dora Maira Massif (Western Alps), two different eclogite- and blueschist-facies units (i.e. the Rocca Solei and Dronero units, respectively), are separated by a shear zone (i.e. the Valmala Tectonic Unit), which
Externí odkaz:
https://doaj.org/article/1817ce2e3c334cc99614855fb8893b25
Publikováno v:
Geosciences, Vol 12, Iss 5, p 212 (2022)
In the present study, we unveil the real significance of mylonitic reworking of the polymetamorphic crystalline basement in the Serre Massif of Calabria (Southern Italy). We use a multidisciplinary approach to comprehend the structural, microstructur
Externí odkaz:
https://doaj.org/article/24d456fccb43400ba68c157308ce4966
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
The Central Balkan Zone belongs to the north-vergent fold-and-thrust belt of the Alpine Balkan orogen. In this zone, pre-Permian low-grade rocks, metamorphosed during the Variscan orogeny, were later reworked at two main stages of the Alpine compress
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c098d99c70f9049fa62498a145b41a69
https://zenodo.org/record/7870556
https://zenodo.org/record/7870556
Autor:
Andrea Festa, Chiara Groppo, Paola Cadoppi, Francesco Nosenzo, Gianni Balestro, Gianfranco Fioraso
Publikováno v:
Journal of Maps, Vol 16, Iss 2, Pp 736-744 (2020)
Journal of maps 16 (2020): 736–744. doi:10.1080/17445647.2020.1824825
info:cnr-pdr/source/autori:Balestro G.[1], Nosenzo F.[2], Cadoppi P.[1], Fioraso G.[3], Groppo C.[1], Festa A.[1]/titolo:Geology of the southern Dora-Maira Massif: insights from a sector with mixed ophiolitic and continental rocks (Valmala tectonic unit, Western Alps)/doi:10.1080%2F17445647.2020.1824825/rivista:Journal of maps/anno:2020/pagina_da:736/pagina_a:744/intervallo_pagine:736–744/volume:16
Journal of maps 16 (2020): 736–744. doi:10.1080/17445647.2020.1824825
info:cnr-pdr/source/autori:Balestro G.[1], Nosenzo F.[2], Cadoppi P.[1], Fioraso G.[3], Groppo C.[1], Festa A.[1]/titolo:Geology of the southern Dora-Maira Massif: insights from a sector with mixed ophiolitic and continental rocks (Valmala tectonic unit, Western Alps)/doi:10.1080%2F17445647.2020.1824825/rivista:Journal of maps/anno:2020/pagina_da:736/pagina_a:744/intervallo_pagine:736–744/volume:16
In the Valmala sector of the southern Dora Maira Massif (Western Alps), two different eclogite- and blueschist-facies units (i.e. the Rocca Solei and Dronero units, respectively), are separated by a shear zone (i.e. the Valmala Tectonic Unit), which
Autor:
Puglisi Diego
Publikováno v:
Geologica Carpathica, Vol 65, Iss 4, Pp 293-305 (2014)
The occurrence of a Lower Cretaceous flysch group, cropping out from the Gibraltar Arc to the Balkans with a very similar structural setting and sedimentary provenance always linked to the dismantling of internal areas, suggests the existence of only
Externí odkaz:
https://doaj.org/article/3129e940609e46bd90c0859d58afc583