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Jaime Almeida

Researcher at University of Lisbon

Publications -  9
Citations -  55

Jaime Almeida is an academic researcher from University of Lisbon. The author has contributed to research in topics: Geology & Subduction. The author has an hindex of 2, co-authored 6 publications receiving 10 citations.

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Self-replicating subduction zone initiation by polarity reversal

TL;DR: In this article , the authors present 3D numerical models of subduction zone initiation by polarity reversal resulting from the arrival of an oceanic plateau at the trench, and show that this process is more likely to occur for old subducting plates and narrow plateaus, and that new subduction zones can form from previous ones in a self-replicating manner.
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Analogue modelling of brittle shear zone propagation across upper crustal morpho-rheological heterogeneities

TL;DR: In this paper, different sand-box analogue modelling experiments were carried out to better understand, not only the shear zone perturbation effect caused by strictly rheologic (viscous-weak) anomaly, but also the one arising from a combined morphological perturbations (i.e., traverse topographic crest).
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A computational diffusion model to study antibody transport within reconstructed tumor microenvironments

TL;DR: A computational and microscopy framework to track and simulate antibody transport within the tumor microenvironment that complements the previously established in vitro models platform is presented and paves the way to the development of a valuable tool to study the influence of different components of the tumormicroenvironment on antibody transport.
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Impact of crustal rheology and inherited mechanical weaknesses on early continental rifting and initial evolution of double graben structural configurations: Insights from 2D numerical models

TL;DR: In this paper , a set of numerical experiments were carried out to investigate the influence of lower crust mechanical weaknesses (weak-seeds) in the early rift nucleation of grabens, while simultaneously assuming different rheological configurations for the extending continental crust.