Zobrazeno 1 - 10
of 40
pro vyhledávání: '"Marie-Noëlle Guilbaud"'
Publikováno v:
Geofísica Internacional, Vol 63, Iss 1, Pp 726-728 (2024)
Monogenetic volcanism is a worldwide phenomenon that occurs in all tectonic and geographic environments, representing an important manifestation of the Earth´s internal dynamics that causes the formation of numerous volcanic edifices distributed ove
Externí odkaz:
https://doaj.org/article/97b5b78275b54471bd4aee1401e2ebba
Autor:
Fanni Vörös, Benjamin van Wyk de Vries, Marie-Noëlle Guilbaud, Tolga Görüm, Dávid Karátson, Balázs Székely
Publikováno v:
Remote Sensing, Vol 14, Iss 23, p 6152 (2022)
Morphometric studies of scoria cones have a long history in research. Their geometry and shape are believed to be related to evolution by erosion after their formation, and hence the morphometric parameters are supposed to be related with age. We ana
Externí odkaz:
https://doaj.org/article/06b1b4efc34143808025748ad46f304b
Autor:
Katrin Sieron, Marie-Noëlle Guilbaud, María Cristina Zarazúa-Carbajal, Sergio Francisco Juárez Cerrillo
Publikováno v:
Bulletin of Volcanology. 85
Autor:
Marie-Noëlle Guilbaud, Corentin Chédeville, Ángel Nahir Molina-Guadarrama, Julio Cesar Pineda-Serrano, Claus Siebe
Publikováno v:
Geological Society, London, Special Publications. 520:165-189
The eruption of the c. 10 km 3 rhyolitic Las Derrumbadas twin domes about 2000 years ago generated a wide range of volcano-sedimentary deposits in the Serdán-Oriental lacustrine basin, Trans-Mexican Volcanic Belt. Some of these deposits have been qu
Publikováno v:
Revista Mexicana de Ciencias Geológicas. 38:101-121
Scoria cones are abundant in most volcanic fields on Earth, such as the Michoacán-Guanajuato Volcanic Field, in the central-western sector of the Trans-Mexican Volcanic Belt. However, there are few in-depth studies on their eruptive style and contro
Autor:
Sergio Salinas, Christine Rasoazanamparany, Renato Castro Govea, Marie-Noëlle Guilbaud, Elisabeth Widom, Claus Siebe
Publikováno v:
Journal of Petrology. 60:2317-2338
The origin of the large diversity of rock types erupted along the subduction-related Trans-Mexican Volcanic Belt (TMVB) remains highly debated. In particular, several hypotheses have been proposed to explain the contemporary eruption of calc-alkaline
Publikováno v:
The Holocene. 30:402-419
The Serdán-Oriental lacustrine basin in the eastern part of the Trans-Mexican Volcanic Belt holds a volcanic field of >30 monogenetic vents. Among them, the ~1000-m-high, ~11 km3 Las Derrumbadas rhyolite twin domes dominate the interior of the basin
Autor:
Nayeli Pérez-Rodríguez, Juan Morales, Rubén Cejudo, Marie-Noëlle Guilbaud, Avto Goguitchaichvili
Publikováno v:
Physics of the Earth and Planetary Interiors. 332:106927
Autor:
Benjamin van Wyk de Vries, María del Pilar Ortega-Larrocea, José Alfredo Járquin Rojas, Naara López Velásquez, Silke Cram, Marie-Noëlle Guilbaud
Geological elements in cities are usually damaged and invisible to their inhabitants, despite the wide range of benefits they provide to them. In particular, they offer them an opportunity to learn about their geological setting (= sense of place) an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0e83b16b6ef923babc749fa2d90ddfec
https://doi.org/10.5194/egusphere-egu21-6650
https://doi.org/10.5194/egusphere-egu21-6650
Autor:
Marie-Noëlle Guilbaud, María del Pilar Ortega-Larrocea, Benjamin van Wyk de Vries, Silke Cram
Publikováno v:
Geoheritage
Geoheritage, 2021, 13 (6), ⟨10.1007/s12371-020-00525-9⟩
Geoheritage, Springer, 2021, 13 (6), ⟨10.1007/s12371-020-00525-9⟩
Geoheritage, 2021, 13 (6), ⟨10.1007/s12371-020-00525-9⟩
Geoheritage, Springer, 2021, 13 (6), ⟨10.1007/s12371-020-00525-9⟩
co-auteur étranger; International audience; The conservation of geosites in a region can foster its sustainability and develop geotourism. These geosites provide geoeducation, raise people's awareness on natural hazards and increase their resilience
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::800c4b10f58fc51b87630720de771277
https://hal.science/hal-03118765
https://hal.science/hal-03118765