GERTISSER, R., SELF, S., KELLEY, S.P., GASPAR, J.L., PACHECO, J.M., PIMENTEL, A., QUEIROZ, G. (2005) - A Chronological Framework for Young ( Ilha Terceira|bbce621b-0178-4679-821b-aa7c7f9d19cc
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em encontros internacionais|c2bd86e8-9a16-425b-979d-5e7be7ffeb5f
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Todas as Categorias (Publicação):Painéis:em encontros internacionais
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http://www.cvarg.azores.gov.pt/publicacoes/Paginas/cms_554_GERTISSER-R-SELF-S-KELLEY-S-P-GASPAR-J-L-PACHECO-J-M-PIMENTEL-A-QUEIROZ-G-2005-A-Chronological-Framework-for-Young.aspx
SELF, S., GERTISSER, R., PIMENTEL, A., KELLEY, S.P. (2005) - Calderas and ignimbrites on Terceira, Azores. Proceedings of the Workshop on "Caldera volcanism: analysis, modelling and response", p. 14. Ilha Terceira|bbce621b-0178-4679-821b-aa7c7f9d19cc
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Internacionais|5eff17ae-f420-4d5f-b3cf-a849f6910529
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Todas as Categorias (Publicação):Artigos em livros de actas:Internacionais
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http://www.cvarg.azores.gov.pt/publicacoes/Paginas/cms_175_SELF-S-GERTISSER-R-PIMENTEL-A-KELLEY-S-P-2005-Calderas-and-ignimbrites-on-Terceira-Azores-Proceedings-of-the-Works.aspx
OKADA, J., D' ARAÚJO, J., BONFORTE, A., GUGLIELMINO, F., LORENZO, M., FERREIRA, T. (2016) - Volcanic deformation sources associated with Fogo 2011-2012 unrest, Azores the first modelling result. European Geosciences Union General Assembly 2016, Vienna. em encontros internacionais|c2bd86e8-9a16-425b-979d-5e7be7ffeb5f
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Todas as Categorias (Publicação):Painéis:em encontros internacionais
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Volcanic deformation is often observed at many
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http://www.cvarg.azores.gov.pt/publicacoes/Paginas/pei-egu2016-okada.aspx
em Vulcanologia e Avaliação de Riscos
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Ilhas do grupo Oriental em alerta laranja referente a precipitação (SRPCBA/IPMA)
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Ilhas do grupo Ocidental em alerta amarelo referente a agitação
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http://www.cvarg.azores.gov.pt/loja/Paginas/downloads.aspx
this first phase of the project, the result was a 3-channel portable digital seismic station
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As the result of the co-operation between researchers from Portuguese and Spanish
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http://www.cvarg.azores.gov.pt/publicacoes/Paginas/cms_312_MONTALVO-A-ABRIL-M-WALLENSTEIN-N-ORTIZ-R-2004-Desenvolvimento-de-uma-estacao-sismica-digital-portatil-pela-integra.aspx
this first phase of the project, the result was a 3-channel portable digital seismic station
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As the result of the co-operation between researchers from Portuguese and Spanish
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http://www.cvarg.azores.gov.pt/publicacoes/Paginas/cms_538_MONTALVO-A-ABRIL-M-WALLENSTEIN-N-ORTIZ-R-2004-Integracao-de-sistemas-de-monitorizacao-sismovulcanica-para-o-desenv.aspx
internacionais com arbitragem|4d359cd0-65d2-4abd-8d66-f2d4ecb10cc4
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of primary minerals of volcanic rocks. As a result, water facies range from Na–Cl to Na–HCO3
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http://www.cvarg.azores.gov.pt/publicacoes/Paginas/cms_800_CRUZ-J-V-AMARAL-C-2004-Major-ion-chemistry-of-groundwaters-from-perched-water-bodies-at-Azores-Portugal-volcanic-a.aspx
PIMENTEL, A., SELF, S., PACHECO, J, JEFFERY, A., GERTISSER, R. (2018) – Eruption, deposition and geometry of peralkaline ignimbrites on Terceira, Azores: the case of the Lajes-Angra Ignimbrite Formation. EGU General Assembly 2018, Viena (Áustria). of the two ignimbrites are interpreted to result from differences in the erupted volumes
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of ignimbrite. These ignimbrite formations can result from a single eruption or, more often
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http://www.cvarg.azores.gov.pt/publicacoes/Paginas/coei-egu2018-pimentel-2.aspx
Outras|880649df-c4ac-4efd-b959-5619703341e7
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Doutoramento|2ee09eee-db6d-42ff-9190-8e7ff1d4ee2f
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TFZ, in particular in Skjalfandi Bay. The final result is a map of the seafloor lithology as
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http://www.cvarg.azores.gov.pt/publicacoes/Paginas/cms_283_RIEDEL-C-2001-Self-organizing-seafloor-mapping-of-the-Tjoernes-Fracture-Zone-Dissertation-for-Doktor-der-Naturwiss.aspx
center. The more evolved rocks result essentially from fractional crystallization on
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suggests that This Central Group island result from a single mantelic source, to which HIMU
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http://www.cvarg.azores.gov.pt/publicacoes/Paginas/cms_1037_FRANcA-Z-CRUZ-J-V-NUNES-J-FORJAZ-V-H-2003-Azores-historical-eruptions-geochemical-features-and-related-eruptive-s.aspx