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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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The evolution of cicada songs contrasted with the relationships inferred from mitochondrial dna (insecta, hemiptera)

TL;DR: The observed similarities between the molecular phylogeny and the basic tymbal cycles seem to reflect the basic conservative nature of the tymbAL structure, while the discrepancy between the former and the calling song pattern is probably related to the high plasticity of the pattern generator in the central nervous system and dependent on species-specific selection.
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Anisotropy of magnetic susceptibility constraints on Variscan obduction processes in the Bragança Massif (NE Portugal)

TL;DR: In this article, an anisotropy of magnetic susceptibility (AMS) and structural study of high-grade metamorphic and ophiolitic rocks from the Braganca Massif is presented to contribute to the debate concerning the identification of transport directions during the closure of the Variscan Ocean.
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Erratum to Identification of tsunami-induced deposits using numerical modeling and rock magnetism techniques: A study case of the 1755 Lisbon tsunami in Algarve, Portugal: [Physics of the Earth and Planetary Interiors Volume 182, Issues 3–4, Pages 187–198 (October 2010)]

TL;DR: In this paper, the authors proposed an approach to identify tsunami-induced deposits by combining numerical simulation and rock magnetism, which was tested on the Boca do Rio estuary generated by the 1755 earthquake in Lisbon.
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Exploring Offshore Sediment Evidence of the 1755 CE Tsunami (Faro, Portugal): Implications for the Study of Outer Shelf Tsunami Deposits

TL;DR: In this paper, a multidisciplinary approach was performed to detect the sedimentary imprints left by the 1755 CE tsunami in two cores, located in the southern Portuguese continental shelf at water depths of 58 and 91 m.