3-D geometry reconstruction using a color image stereo pair and partial differential equations

[EN] In this work, we present a new model for a dense disparity estimation and the 3-D geometry reconstruction using a color image stereo pair. First, we present a brief introduction to the 3-D Geometry of a camera system. Next, we propose a new model for the disparity estimation based on an energy functional. We look for the local minima of the energy using the associate Euler-Langrage partial differential equations. This model is a generalization to color image of the model developed in, with some changes in the strategy to avoid the irrelevant local minima. We present some numerical experiences of 3-D reconstruction, using this method some real stereo pairs.

Evolución geomorfológica de la superficie de erosión R1000 en los Llanos de Castro Caldelas (Ourense)

[ES] Se presenta el análisis morfológico de un sector del replano RIOOO' El sector escogido está colgado por encima de la red fluvial actual. Este hecho permite atribuir a los cursos que drenan el replano un carácter semi funcional. Se han identificado once niveles de terrazas erosivas, que corresponden al desmantelamiento del replano inicial. La geometría de la red permite suponer que la organización actual se alcanzó mediante sucesivas capturas. Por otra parte, se han distinguido dos trazados de la red (centrípeta y en bayoneta); la red centrípeta define una superficie hueca y la red en bayoneta una superficie en rampas escalonadas. Se propone que ambas morfologías corresponderían a diferentes estadios de un mismo proceso: el vaciado del RIOOO' Por último, se propone la hipótesis de un descabalamiento tectónico del Rgoo para el origen de los Llanos.

Evolución geomorfológica del Macizo Hespérico peninsular:estudio de un sector comprendido entre las provincias de Lugo y Ourense (Galicia, NW de España)

[EN] This paper deals with the relief generation in Ourense, an interior territory of the Galicia Country, at NW Spain, after the breakdown of Pangea 200 million years ago. The rupture of supercontinent causes the main effects in the outer part of Galicia, the present coast line and the shelf, but also the inner parts of Galicia where the landscape changes dramatically mainly ruled by fluvial incision connected with uprising, (orogenic, epirogenic, or isostatic origin), or even with eustatic oscillations, that shaped the previous old mesozoic landscape. Various things complicate the correct understanding of Galician geomorphology:1) the prevalent hercynian structure, (presumably reactivated during the Alpine Orogeny), causes that the epigenic processes, (fluvial, glaciar, marine and etching), acting on Galicia from Mesozoic to present times, produce end forms identified erroneously at the previous literature as tectonic and not as etch forms profiting from lithological or structural contrasts. 2) the common morphotectonic model accepted by all previous researchers establishes for the whole of Galicia a blocky pattern, (horst and graben like), due to extensional tectonic regime. This model is proved as no longer valid because the Galician tertiary basins, even were described at the past as graben depressions never have this origin. 3) big differences exist between the north and western sides of Galicia that show contrasted tectonic regime: compressional (with forms as the so called raised platforms), at the northern coast border, and extensional (with forms so typical as the Rias), at the western side. The study area is located at the confluence of two tectonic domains where the above mentioned effects are coincidents and specially well showed through different effects: prominent assimetry of fluvial captures (west facing), pronounced river incision and different kinds of tertiary basins: either strike slipe faults (Maceda, Xinzo de Limia, etc), or overslipped by inverse faults, (Quiroga, A Rúa, etc.), or even corresponding with depressions never, (or anywise passively), affected by tectonic movements, (Monforte). The paper include a detailed inventory of surfaces and terrace levels and their incision sequence which allow stablish a relative chronology of geomorphic evolution at this area of NW Spain during meso-cainozoic times.

Caracterización computacional de un detector de germanio hiperpuro de rango extendido (HPGe- XtRa) con simulación Montecarlo y optimización con un algoritmo evolutivo

Máster Universitario en Sistemas Inteligentes y Aplicaciones Numéricas en Ingeniería (SIANI)