Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Gabriel Ureta"'
Publikováno v:
Geosciences, Vol 10, Iss 12, p 507 (2020)
Maar volcanoes are monogenetic landforms whose craters cut below the pre-eruptive surface and are surrounded by a tephra ring. Both the maar crater and the surrounding tephra rim deposits are typically formed due to magma–water explosive interactio
Externí odkaz:
https://doaj.org/article/3fe963d415724ec0bcfda26347ab973d
Autor:
Felipe Aguilera, Susana Layana, Felipe Rojas, Pilar Arratia, Thomas C. Wilkes, Cristóbal González, Manuel Inostroza, Andrew J.S. McGonigle, Tom D. Pering, Gabriel Ureta
Publikováno v:
Remote Sensing, Vol 12, Iss 13, p 2122 (2020)
UV cameras have been used for over a decade in order to remotely sense SO2 emission rates from active volcanoes, and to thereby enhance our understanding of processes related to active and passive degassing. Whilst SO2 column density retrievals can b
Externí odkaz:
https://doaj.org/article/1ebc2671d6f7425b96066f25e567a7c8
Autor:
Pablo Grosse, Martin Danišík, Facundo D. Apaza, Silvina R. Guzmán, Pierre Lahitte, Xavier Quidelleur, Stephen Self, Claus Siebe, Benjamin van Wyk de Vries, Gabriel Ureta, Marcel Guillong, Rosanna De Rosa, Petrus Le Roux, Jörn-Frederik Wotzlaw, Olivier Bachmann
Publikováno v:
Bulletin of Volcanology
Bulletin of Volcanology, 2022, 84, ⟨10.1007/s00445-022-01594-0⟩
Bulletin of Volcanology, 2022, 84, ⟨10.1007/s00445-022-01594-0⟩
International audience; Volcano sector collapses are catastrophic events that can mobilize huge volumes of material and cause changes in the magmatic plumbing system, leading to variations in growth rate and/or composition. Dating pre-historic volcan
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::62d801ba704c38e81f406d4836753ba0
https://doi.org/10.1007/s00445-022-01594-0
https://doi.org/10.1007/s00445-022-01594-0
Autor:
Felipe Aguilera, Fredy Apaza, José Del Carpio, Pablo Grosse, Néstor Jiménez, Gabriel Ureta, Manuel Inostroza, Walter Báez, Susana Layana, Cristóbal Gonzalez, Marco Rivera, Mayra Ortega, Rodrigo Gonzalez, Rodrigo Iriarte
Publikováno v:
Bulletin of Volcanology. 84
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0a643bb1454d582f4421c928a845e29b
https://doi.org/10.1007/s00445-022-01526-y
https://doi.org/10.1007/s00445-022-01526-y
Autor:
Jorge E. Romero, Gabriel Ureta, Paulina Fuentes, Alexandre Corgne, José A. Naranjo, Carlos F. Ramírez, Boris Chako-Tchamabé, Miguel Cáceres, José Lazcano
Publikováno v:
Journal of Volcanology and Geothermal Research. 429:107618
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7e515e8daecff2cd280ef6d28a535526
https://doi.org/10.1016/j.jvolgeores.2022.107618
https://doi.org/10.1016/j.jvolgeores.2022.107618
Autor:
José Pablo Sepúlveda, Mauricio Aguilera, Matias Vilches, Gabriel Ureta, Alexander Scheinost, Ivana Torres, Károly Németh, Felipe Aguilera, Rodrigo Stumpf González
Monogenetic volcanism produces small eruptive volumes with short eruption history, different chemical compositions, and relatively simple conduit. The Central Volcanic Zone of the Andes is internationally known as a natural laboratory to study volcan
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d82aee277744f3742826cec299074d4e
https://doi.org/10.5772/intechopen.93959
https://doi.org/10.5772/intechopen.93959
Publikováno v:
Bulletin of Volcanology
Cerro Overo maar and La Albondiga lava dome are two independent monogenetic volcanoes located in the Central Volcanic Zone of the Andes in northern Chile, close to the active Lascar and Chiliques volcanoes. Cerro Overo maar was formed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cedc7dd7ba1e3cc58ec9ec5eb8ce2d15
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5006041
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5006041
Publikováno v:
Geosciences, Vol 10, Iss 507, p 507 (2020)
Geosciences
Volume 10
Issue 12
Geosciences
Volume 10
Issue 12
Maar volcanoes are monogenetic landforms whose craters cut below the pre-eruptive surface and are surrounded by a tephra ring. Both the maar crater and the surrounding tephra rim deposits are typically formed due to magma&ndash
water explosive i
water explosive i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f12aec7d29e1531b41a06788557c322b
https://www.mdpi.com/2076-3263/10/12/507
https://www.mdpi.com/2076-3263/10/12/507
Autor:
Károly Németh, Martin Zimmer, Cristóbal González, Manuel Inostroza, Felipe Aguilera, Gabriel Ureta, Andrew Menzies
Publikováno v:
Journal of South American Earth Sciences
Cerro Tujle is an isolated Quaternary maar located 21 km south-east of the Salar de Atacama basin. It is situated at 3,554 m a.s.l., on the top of the Cordon de Tujle ridge forming a north-south striking morphological element in the Central Volcanic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f830e89ccc8470e855869b2736e8169e
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5003441
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5003441
Autor:
Mauricio Aguilera, Gabriel Ureta, Pablo Grosse, Károly Németh, Felipe Aguilera, Matias Vilches
Publikováno v:
Journal of Volcanology and Geothermal Research. 422:107458
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0d36b412ed5e4eee382120f11a9fd223
https://doi.org/10.1016/j.jvolgeores.2021.107458
https://doi.org/10.1016/j.jvolgeores.2021.107458