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Pedro Silva

Researcher at University of Lisbon

Publications -  39
Citations -  807

Pedro Silva is an academic researcher from University of Lisbon. The author has contributed to research in topics: Volcano & Lava. The author has an hindex of 16, co-authored 38 publications receiving 737 citations. Previous affiliations of Pedro Silva include Instituto Politécnico Nacional & Instituto Superior de Engenharia de Lisboa.

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Multi-stage evolution of a sub-aerial volcanic ridge over the last 1.3 Myr: S. Jorge Island, Azores Triple Junction

TL;DR: In this paper, K/Ar dating and geochemical analyses have been carried out on the WNW-ESE elongated oceanic island of S. Jorge to reconstruct the volcanic evolution of a linear ridge developed close to the Azores triple junction.

Reconstructing the architectural evolution of volcanic islands from combined K/Ar, morphologic, tectonic, and magnetic data: the Faial Island example (Azores)

TL;DR: In this paper, a multi-disciplinary study of the successive stages of development of Faial (Azores) during the last 1 Myr is presented, using high-resolution digital elevation model (DEM), and new K/Ar, tectonic, and magnetic data, in response to complex interactions between volcanic construction and mass wasting, including the development of a graben.
Journal ArticleDOI

Reconstructing the architectural evolution of volcanic islands from combined K/Ar, morphologic, tectonic, and magnetic data: The Faial Island example (Azores)

TL;DR: In this article, a multi-disciplinary study of the successive stages of development of Faial (Azores) during the last 1 Myr is presented, using high-resolution digital elevation model (DEM), and new K/Ar, tectonic, and magnetic data, in response to complex interactions between volcanic construction and mass wasting, including the development of a graben.
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Mantle source heterogeneity, magma generation and magmatic evolution at Terceira Island (Azores archipelago):: Constraints from elemental and isotopic (Sr, Nd, Hf, and Pb) data

TL;DR: In this article, the present-day mantle heterogeneity in the Azores region through the study of two active volcanic systems from Terceira Island is addressed, and it is shown that mantle heterogeneities are detectable even when “coeval” volcanic systems (Santa Barbara and Fissural) erupted less than 10 km away.