Regimen interno y potestad disciplinaria aplicable en los centros de internamiento de menores con medidas judiciales. Experiencias prácticas y correcta interpretación y aplicación del reglamento de menores

[ES] El trabajo que presentamos presenta una línea pedagógica jurídica educativa, garantista de los derechos y deberes de los jóvenes con medidas judiciales en la aplicación del Real Decreto 1774/2004, de 30 de julio, por el que se aprueba el Reglamento de la Ley Orgánica 5/2000, de 15 de enero Reguladora de la Responsabilidad Penal del Menor. Se orienta en la buena praxis y aplicación del Reglamento, realizando una combinación de la experiencia, de los marcos legales de Justicia Juvenil y de Instituciones Penitenciarias.

Morphogenesis of the Ourense plains:(NW of Spain)

[EN] We present a geomorphological analysis of Ourense Province (NW Spain) characterized by: a general narrowing of the fluvial network, highlands with smooth reliefs partially eroded and lowlands with residual reliefs, several extensive plains of erosion frequently limited by fractures -among which Tertiary grabens are inserted-, some ?Hollow Surface?-type morphology, absence of sedimentary deposits outside the grabens, and a generalized outcrop of the Hercynian Massif substratum. Traditionally, this ?piano?s keyboard morphology? has been interpreted as expression of block tectonics in tensile regimen; instead we suggest the existence of: an isostatic upheaval simultaneous to a sequence of tectonic pulses of compressive regimen with activity in favour of transcurrent faults, a General Surface (R600), several plains that present a ?Hollow Surface?-type morphology (R1600 R1400 R1000), a generalized alteration that correspond to a same process of decomposition associated to fluctuating conditions of redox equilibrium, a erosional terraces related principaly to the palaeo-fluvial nets; moreover, we propose the existence of two morphoestructural lineament: the first one represented by the Fault of Vila Real (NE-SW) -a ramification of the ?Basal Pyrenean Overthrust?-, that would have been active at an early moment of the tectonic sequence with a left transcurrent fault, secondly the lineament represented by the Fault of Maceda (NNW-SSE) that would be related to the ?Fault System NW-SE? and would have produced a right transcurrent fault during a late tectonic pulse.