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Pedro P. Cunha

Researcher at University of Coimbra

Publications -  230
Citations -  3642

Pedro P. Cunha is an academic researcher from University of Coimbra. The author has contributed to research in topics: Medicine & Fluvial. The author has an hindex of 30, co-authored 196 publications receiving 3007 citations. Previous affiliations of Pedro P. Cunha include University of Lisbon.

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Early vascular ageing in translation: from laboratory investigations to clinical applications in cardiovascular prevention.

TL;DR: An update is given on EVA and how the concept can be used in clinical practice, a condition that could increase cardiovascular risk and is associated with various degrees of cognitive dysfunction, as well as other features of biological ageing.
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MiRNA-21 silencing mediated by tumor-targeted nanoparticles combined with sunitinib: A new multimodal gene therapy approach for glioblastoma.

TL;DR: Results provide evidence that CTX-coupled SNALPs are a reliable and efficient system for systemic delivery of anti-miRNA oligonucleotides and suggest that miRNA modulation by the targeted nanoparticles combined with anti-angiogenic chemotherapy may hold promise as an attractive approach towards GBM treatment.
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The Use of Multiple Correspondence Analysis to Explore Associations between Categories of Qualitative Variables in Healthy Ageing.

TL;DR: MCA provided a powerful tool to explore complex ageing data, covering multiple and diverse variables, showing if a relationship exists and how variables are related, and offering statistical results that can be seen both analytically and visually.
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Dating the Tejo river lower terraces in the Ródão area (Portugal) to assess the role of tectonics and uplift

TL;DR: In this paper, a chronological framework for the Tejo river terraces is established by integrating geomorphological, stratigraphical and archaeological information with ages from luminescence dating.
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Tectonic classification of Cenozoic Iberian foreland basins

TL;DR: In this article, a simple evolutionary model shows a migration from East to West, in which basins are still tectonically active at the Atlantic margin of Iberia, and the common evolution is also found in a series of geometrical characteristics, such as the ratio r of length of strike-slip fault and length of thrust fault.