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Reply to the comment by Quartau and Mitchell on “Reconstructing the architectur...

Hildenbrand, Anthony; Marques, Fernando; Costa, A.; Sibrant, A.; Silva, Pedro; Henry, Bernard; Miranda, Jorge Miguel; Madureira, Pedro

Reply to the comment by Quartau and Mitchell on “Reconstructing the architectural evolution of volcanic islands from combined K/Ar, morphologic, tectonic, and magnetic data: The Faial Island example (Azores)”, J. Volcanol. Geotherm. Res. 241–242, 39–48, by Hildenbrand et al. (2012)


Reconstructing the architectural evolution of volcanic islands from combined K/...

Hildenbrand, Anthony; Marques, Fernando; Costa, A.; Sibrant, A.L.R.; Silva, Pedro; Henry, Bernard; Miranda, Jorge; Madureira, Pedro

The morpho-structural evolution of oceanic islands results from competition between volcano growth and partial destruction by mass-wasting processes. We present here a multi-disciplinary study of the successive stages of development of Faial (Azores) during the last 1 Myr. Using high-resolution digital elevation model (DEM), and new K/Ar, tectonic, and magnetic data, we reconstruct the rapidly evolving topograp...


Reconstructing the architectural evolution of volcanic islands from combined K/...

Hildenbrand, Anthony; Marques, Fernando; Costa, A.C.G.; Sibrant, A.L.R.; SIlva, Pedro; Henry, Bernard; Miranda, Miguel; Madureira, Pedro

The morpho-structural evolution of oceanic islands results from competition between volcano growth and partial destruction by mass-wasting processes. We present here a multi-disciplinary study of the successive stages of development of Faial (Azores) during the last 1 Myr. Using high-resolution digital elevation model (DEM), and new K/Ar, tectonic, and magnetic data, we reconstruct the rapidly evolving topograp...


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    Financiadores do RCAAP

Fundação para a Ciência e a Tecnologia Universidade do Minho   Governo Português Ministério da Educação e Ciência Programa Operacional da Sociedade do Conhecimento União Europeia