Fault-volcano interactions with broadly distributed stretching in rifts

Autor: De Matteo A.[1], Corti G.[2, Van Wyk De Vries B.[4], Massa B.[1, Mussetti G. [6]

Publikováno v: Journal of Volcanology and Geothermal Research
Journal of Volcanology and Geothermal Research, 2018, 362, pp.64-75. ⟨10.1016/j.jvolgeores.2018.08.008⟩
Journal of volcanology and geothermal research 362 (2018): 64–75. doi:10.1016/j.jvolgeores.2018.08.008
info:cnr-pdr/source/autori:De Matteo A.[1], Corti G.[2,3], Van Wyk De Vries B.[4], Massa B.[1,5], Mussetti G. [6]/titolo:Fault-volcano interactions with broadly distributed stretching in rifts/doi:10.1016%2Fj.jvolgeores.2018.08.008/rivista:Journal of volcanology and geothermal research/anno:2018/pagina_da:64/pagina_a:75/intervallo_pagine:64–75/volume:362

Areas undergoing pure extension are typically characterized by the formation of faults and fractures orthogonal to the maximum principal stress. In these conditions, the presence of a volcano and its magmatic system perturbs the local stress field, l

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::319ed2b70920ce9aba8229fc06bfe761
https://doi.org/10.1016/j.jvolgeores.2018.08.008