Zobrazeno 1 - 10
of 23
pro vyhledávání: '"Alessandro Decarlis"'
Autor:
Francesco Arboit, Kerstin Drost, Alessandro Decarlis, David Chew, Dominik Hennhoefer, Andrea Ceriani
Publikováno v:
Scientific Reports, Vol 13, Iss 1, Pp 1-14 (2023)
Abstract The Cenozoic succession of the Jabal Hafeet anticline yields the most complete surface expression of the deformation that affected the Southeast Arabian Foreland Basin (SEAFB). The carbonate rocks of the Eocene Rus Formation comprise the cor
Externí odkaz:
https://doaj.org/article/5847787ee6754e479e26955dd0a075d8
Autor:
Gianreto Manatschal, Pauline Chenin, Isabelle Haupert, Emmanuel Masini, Gianluca Frasca, Alessandro Decarlis
Publikováno v:
Geosciences, Vol 12, Iss 12, p 434 (2022)
We reassess the architecture and tectonic history of the Western Alps based on recent knowledge developed at rifted margins. First, we replace the main Alpine units of our study area into a synthetic rifted margin template based on diagnostic petrolo
Externí odkaz:
https://doaj.org/article/0356a0cf27c040dca7ef9b1472f0a8fb
Autor:
Abimbola Chris Ogunyele, Mattia Bonazzi, Alessio Sanfilippo, Alessandro Decarlis, Alberto Zanetti
The Ivrea-Verbano Zone (IVZ) is the westernmost sector of the Southern Alps. It is constituted by granulite-to-amphibolite-facies continental crust representing the basement of the Adria plate. The IVZ contains many orogenic mantle peridotites. The l
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::199b591e567f2cfdc746b6e5b7d75d67
https://doi.org/10.5194/egusphere-egu23-243
https://doi.org/10.5194/egusphere-egu23-243
Publikováno v:
Sedimentology. 69:1675-1704
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4e3add3fed77bf1404633233131e891d
https://doi.org/10.1111/sed.12968
https://doi.org/10.1111/sed.12968
Publikováno v:
Journal of the Geological Society. 180
The formation of oceanic crust in the southern and central Red Sea is generally accepted to have started at c. 5 Ma. However, the nature of the crust in the northern Red Sea is still debated. This paper describes the rift architecture, dynamics and e
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::473ca4b905b83b85004733a390171872
https://doi.org/10.1144/jgs2022-105
https://doi.org/10.1144/jgs2022-105
Autor:
Andrea Ceriani, Chiara Amadori, Thomas Steuber, Andrea Di Giulio, Francesco Arboit, Alessandro Decarlis, Aisha Al Suwaidi
Publikováno v:
Basin Research. 34:555-569
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d9936e77f1cf8c6af743c1394c6b0e50
https://doi.org/10.1111/bre.12630
https://doi.org/10.1111/bre.12630
Autor:
Moamen Ali, Marco Ligi, Andrea Ceriani, Fateh Bouchaala, William Bosworth, Alessandro Decarlis
Publikováno v:
Tectonics. 41
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a62a3497d901258b6f8d3ae072d5696a
https://doi.org/10.1029/2022tc007228
https://doi.org/10.1029/2022tc007228
Autor:
Alessandro Decarlis, Alberto Zanetti, Abimbola Chris Ogunyele, Andrea Ceriani, Riccardo Tribuzio
Publikováno v:
Earth-Science Reviews. 238:104318
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::810ba2c856617a317d6062731c617d33
https://doi.org/10.1016/j.earscirev.2023.104318
https://doi.org/10.1016/j.earscirev.2023.104318
Autor:
Laura Gaggero, Finlay M. Stuart, Alessandro Decarlis, Marco Beltrando, Simona Ferrando, Gianreto Manatschal, Maria Giuditta Fellin, Matteo Maino, Silvio Seno
Publikováno v:
Tectonics. 36:3209-3228
The thermal evolution of distal domains along rifted margins is at present poorly constrained. In this study, we show that a thermal pulse, most likely triggered by lithospheric thinning and asthenospheric rise, is recorded at upper crustal levels an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2274ba4a4befc8b8664e8df2f2b6001d
https://doi.org/10.1002/2017tc004634
https://doi.org/10.1002/2017tc004634
Publikováno v:
Tectonics. 36:2388-2406
The Alpine Tethys rifted margins were generated by a Mesozoic polyphase magma-poor rifting leading to the opening of the Piedmont-Ligurian “Ocean”. This latter developed through different phases of rifting that terminated with the exhumation of s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::67ef7b9ddb1bdc01d397c4dbc683e664
https://doi.org/10.1002/2017tc004561
https://doi.org/10.1002/2017tc004561