Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Juan Camilo Meza-Cala"'
Autor:
Juan Camilo Meza-Cala, Alexander Minakov, Jan Inge Faleide, Mansour M. Abdelmalak, Grace E. Shephard, Rune Mattingsdal, Wolfram H. Geissler, Carmen Gaina
Publikováno v:
Communications Earth & Environment, Vol 5, Iss 1, Pp 1-10 (2024)
Abstract Intraplate volcanism has occurred for the last 35 million years within Northeast Atlantic and Arctic margins, including the western Barents Sea, Svalbard, and northern Greenland. Earlier studies have suggested that some of this volcanism mig
Externí odkaz:
https://doaj.org/article/857b6665724647849216cd67bbc3d5c1
Publikováno v:
Basin Research.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c3849c073d20d31efe4c8e660d21c1f1
https://doi.org/10.1111/bre.12756
https://doi.org/10.1111/bre.12756
Autor:
Carolina Ortiz-Guerrero, Camilo Montes, David W. Farris, Catalina Agudelo, Margarita Ariza Acero, Juliana Ayala, Jose David Avellaneda, Alejandro Cortes-Calderon, Esteban Gaitan, Sebastian Garzon, Daniel Gongora-Blanco, Nubia Andrea Jara, Juan Camilo Meza-Cala, Lina Perez-Angel, Nathalia Pineda-Rodríguez, Alejandro Rodriguez-Parra, Billy Revelo-Obando, Carolina Rubiano, Elena Stiles, Maria Paz Urdaneta, Nicolas Zuluaga, Felipe Lamus, Federico Moreno, Aldo Rincon
Publikováno v:
International Geology Review (2023)
International Geology Review
International Geology Review
Detailed geologic mapping (639 field stations in ~700 km2) and a ~50 km-long gravity survey (142 stations) in the western Azuero Peninsula revealed two faulted and folded slivers of oceanic crust attached to the trailing edge of the Caribbean Large I
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2f29f058dd4e49ccb046c93b217db7bb
https://doi.org/10.1080/00206814.2023.2191678
https://doi.org/10.1080/00206814.2023.2191678
Autor:
Filippos Tsikalas, Juan Camilo Meza-Cala, Mohamed Mansour Abdelmalak, Jan Inge Faleide, Harald Brekke
Publikováno v:
Geological Society, London, Memoirs. 57
The Lofoten Rifted Margin is a composite tectono-sedimentary element (CTSE), located offshore northern Norway, and comprises the northernmost part of the Norwegian Sea margin at its transition to the West Barents Sea margin. We refine the late Paleoz
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::83aa408b45ee366b803018e6ef8214c0
https://doi.org/10.1144/m57-2021-43
https://doi.org/10.1144/m57-2021-43