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pro vyhledávání: '"Marina Nebot"'
Autor:
Joan Guimerà, Marina Nebot
Publikováno v:
Geological Magazine. 155:630-640
The Maestrat basin was one of the most subsident basins of the Mesozoic Iberian Rift system, developed by a normal fault system which divided it into sub-basins. Its Cenozoic inversion generated the N-verging Portalrubio–Vandellòs fold-and-thrust
Autor:
Francesc Sàbat, Ramón Mas, Ginés A. de Gea, Javier Martín-Chivelet, Consuelo Arias, Pablo Suarez-Gonzalez, Juan Pedro Rodríguez-López, Joan J. Fornós, Luis M. Nieto, José Arribas, Silvia Omodeo-Salé, José Manuel Castro, Antonio Pedrera, Bernadí Gelabert, Beatriz Bádenas, P. A. Ruiz-Ortiz, Rocío Navarrete, Ana Rosa Soria, Isabel Emma Quijada, Marina Nebot, Jesús García-Senz, Ramon Salas, David Garófano, María Luisa Quijano, Maria Eugenia Arribas, Roque Aguado, Carlos L. Liesa, Telm Bover-Arnal, Josep Anton Muñoz, Alejandro Robador, José López-Gómez, Nieves Meléndez, Marcos Aurell, María Isabel Benito, Carlos Peropadre, José Miguel Molina, Idoia Rosales, Laura González-Acebrón, Francisco Coruña, Jordi Giménez, Matías Reolid, Joan Guimerà, Lorenzo Vilas, Antonio Rodríguez-Perea, Antonio M. Casas-Sainz, Marian Fregenal-Martínez
Publikováno v:
The Geology of Iberia: A Geodynamic Approach ISBN: 9783030112943
During the Late Jurassic and Early Cretaceous, Iberia experienced extensional and transtensional stresses leading to a complex rifting time interval. Africa–America–Europe relative motions determined the definition of the Iberian plate boundaries
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::64f08fbf5414a494b178d700cd4dc200
https://doi.org/10.1007/978-3-030-11295-0_5
https://doi.org/10.1007/978-3-030-11295-0_5