2007
DOI: 10.1016/j.tecto.2007.09.001
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Crustal seismic velocity structure near Faial and Pico Islands (AZORES), from local earthquake tomography

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Cited by 50 publications
(44 citation statements)
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“…To date, studies of the islands' seismic structure have only been carried out in limited areas and do not cover the whole Azores Archipelago (e.g. Dias et al 2007). In general, crustal thickness estimates beneath the islands have been in the 10-30 km range (e.g.…”
Section: Introductionmentioning
confidence: 99%
“…To date, studies of the islands' seismic structure have only been carried out in limited areas and do not cover the whole Azores Archipelago (e.g. Dias et al 2007). In general, crustal thickness estimates beneath the islands have been in the 10-30 km range (e.g.…”
Section: Introductionmentioning
confidence: 99%
“…This administrative figure includes and articulates all conservation areas of the island into a single management structure and policy definition system and authority (Fonseca et al, 2011). Geomorphology determines the main characteristics and zonation of the island (Dias et al, 2007). The predominant soils are Andisols.…”
Section: Study Areamentioning
confidence: 99%
“…The Island of Pico, through its morphology, expresses remarkably the effects of volcano-tectonic structures that are in its origin (Nunes, 1999;Madeira & Silveira, 2003;Cruz et al, 2006;França et al, 2006;Dias et al, 2007). Three different areas can be distinguished on the island Nunes, 1999;Madeira & Silveira, 2003;França et al, 2006;Dias et al, 2007): the older volcano (Topo volcano), a central type shield volcano located in the middle-south of the island, is composed of ankaramitic and basaltic lava flows and is partially dismantled by landslides, displaced by faulting and covered by younger volcanism; an intermediate volcanostratigraphic unit, which comprises several alignments of basaltic spatter cones and related lava flows along WNW-ESE fault; and finally the youngest unit of the island is the Madalena Volcanic Complex, which can be structurally divided into two sub-units, the East fissural zone which is composed of several alignments of cinder and spatter cones and related lava flows, and the strato-volcano of Pico displaying a pit crater on its summit and straddling the fissural structure at its western end.…”
Section: Biophysical Information Geologymentioning
confidence: 99%