Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Margherita Fittipaldi"'
Autor:
Laura Parisi, Nico Augustin, Daniele Trippanera, Henning Kirk, Anke Dannowski, Rémi Matrau, Margherita Fittipaldi, Adriano Nobile, Olaf Zielke, Eduardo Valero Cano, Guus Hoogewerf, Theodoros Aspiotis, Sofia Manzo-Vega, Armando Espindola Carmona, Alejandra Barreto, Marlin Juchem, Cahli Suhendi, Mechita Schmidt-Aursch, P. Martin Mai, Sigurjón Jónsson
Publikováno v:
Seismica, Vol 3, Iss 1 (2024)
In the last decades, the slow-spreading Red Sea rift has been the objective of several geophysical investigations to study the extension of the oceanic crust, the thickness of the sedimentary cover, and the formation of transform faults. However, loc
Externí odkaz:
https://doaj.org/article/19a9c9c6c7074ed6ba07cbd14426f821
Autor:
Rémi Matrau, Yann Klinger, Jonathan Harrington, Thorvaldur Thórdarson, Ármann Höskuldsson, Esther Gudmundsdöttir, Laura Parisi, Margherita Fittipaldi, Ulas Avsar, Sigurjón Jónsson
Studies of Oceanic Transform Faults (OTFs) usually rely on geophysical data because of the OTF inaccessibility on the seafloor. The Húsavík-Flatey Fault (HFF) in northern Iceland is an OTF connecting the onshore rift in Iceland to an offshore rift
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5cc9250952729a21d9cf7d074bc1ad84
https://doi.org/10.5194/egusphere-egu23-6567
https://doi.org/10.5194/egusphere-egu23-6567
Autor:
Margherita Fittipaldi, Daniele Trippanera, Nico Augustin, Froukje M. van der Zwan, Alexander Petrovic, Dirk Metz, Sigurjon Jónsson
The Red Sea is a unique place to study a young oceanic rift basin and the interplay between magma and tectonics at a young divergent plate boundary. The spreading rate of the Red Sea rift changes from ~17 mm/yr in the south to ~7 mm/yr in the north,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4fc729a86ca9706fe08a5239c29cef84
https://doi.org/10.5194/egusphere-egu22-11791
https://doi.org/10.5194/egusphere-egu22-11791
Autor:
Nico Augustin, Sigurjón Jónsson, Margherita Fittipaldi, Froukje M. van der Zwan, Daniele Trippanera
The Red Sea is a unique place to study the birth of an oceanic rift basin and the interplay between magma and tectonics at a young divergent plate boundary. The Red Sea is a NNW-SSE oriented and 2000 km long rift system with a spreading rate decreasi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c7502a5f1b17072c79b5fd1963a97352
https://doi.org/10.5194/egusphere-egu2020-9401
https://doi.org/10.5194/egusphere-egu2020-9401