The EU as a foreign policy actor – should human rights really be promoted in China?

La UE promou les seves normes i principis com els drets humans a tercers països també. en aquest document conceptualitza la UE en el seu poder normatiu i presenta la seva política de drets humans i alguns interpretacions alternatives dels drets humans. La qüestió de si, i en el qual el preu de la UE ha de promoure els drets humans a la Xina, tenint en compte diversos punts de conflicte i si es pot complir amb el seu paper d'un poder normatiu a la llum de diferents restriccions s'examinen. Finalment, és analitza el que això implica per a la realització limitada demanda original de la UE i el que un optimitzat. política de drets humans pot semblar

Sedimentary record of the northward flight of India and its collision with Eurasia (Ladakh Himalaya, India)

Stratigraphic and petrographic analysis of the Cretaceous to Eocene Tibetan sedimentary succession has allowed us to reinterpret in detail the sequence of events which led to closure of Neotethys and continental collision in the NW Himalaya. During the Early Cretaceous, the Indian passive margin recorded basaltic magmatic activity. Albian volcanic arenites, probably related to a major extensional tectonic event, are unconformably overlain by an Upper Cretaceous to Paleocene carbonate sequence, with a major quartzarenite episode triggered by the global eustatic sea-level fall at the Cretaceous/Tertiary boundary. At the same time, Neotethyan oceanic crust was being subducted beneath Asia, as testified by calc-alkalic volcanism and forearc basin sedimentation in the Transhimalayan belt. Onset of collision and obduction of the Asian accretionary wedge onto the Indian continental rise was recorded by shoaling of the outer shelf at the Paleocene/Eocene boundary, related to flexural uplift of the passive margin. A few My later, foreland basin volcanic arenites derived from the uplifted Asian subduction complex onlapped onto the Indian continental terrace. All along the Himalaya, marine facies were rapidly replaced by continental redbeds in collisional basins on both sides of the ophiolitic suture. Next, foreland basin sedimentation was interrupted by fold-thrust deformation and final ophiolite emplacement. The observed sequence of events compares favourably with theoretical models of rifted margin to overthrust belt transition and shows that initial phases of continental collision and obduction were completed within 10 to 15 My, with formation of a proto-Himalayan chain by the end of the middle Eocene.

On [summation of 1 raised to the power 1] equivalence relations over the natural numbers

"Vegeu el resum a l'inici del document del fitxer adjunt"

La Insostenibilidad energética del "Gran Dragón": China 1985-2009

China ya no es solo la principal fábrica del mundo, con el consiguiente nivel de consumo de recursos naturales (energía y materiales) y de emisiones de contaminantes, sino que se ha convertido en uno de los principales acreedores mundiales, y como tal, en garante del crecimiento de la mayoría de las economías occidentales. La insostenibilidad del modelo de crecimiento chino, basado en una copia de los países occidentales, se hace más evidente desde la crisis de oferta de petróleo que sacudió al mundo en julio de 2008, con los precios en máximos históricos, y que vino seguida de la crisis financiera en la que todavía nos encontramos. El presente artículo muestra la evolución del consumo de energía en China en los últimos 25 años y presenta algunas posibles causas del mismo, para concluir que es necesario repensar el modelo actual, que incluye las propuestas de salida de la crisis en China y en Occidente. Estas propuestas reiteran en los mismos errores del pasado inmediato, lo que nos puede conducir a una nueva crisis de oferta y a otra financiera, cuyos efectos distributivos a nivel mundial serán más graves que los actuales, a pesar de que puedan implicar una mejora ambiental.

Tectonic evolution of the High Himalaya in upper Lahul (NW Himalaya, India)

The Upper Lahul region in the NW Himalaya is located in the transition zone between the High Himalayan Crystalline (HHC) to the SW and the Tethyan Zone sedimentary series to the NE. The tectonic evolution of these domains during the Himalayan Orogeny is the consequence of a succession of five deformation events. An early D1 phase corresponds to synmetamorphic, NE verging folding. This deformation created the Tandi Syncline, which consists of Permian to Jurassic Tethyan metasediments cropping out in the core of a large-scale synformal fold within the HHC paragneiss. This tectonic event is interpreted as related to a NE directed nappe stacking (Shikar Beh Nappe), probably during the late Eocene to the early Oligocene. A subsequent D2a phase caused SW verging folding in the HHC. This deformation is interpreted as contemporaneous with late Oligocene to early Miocene SW directed thrusting along the Main Central Thrust. In the Tethyan Zone, a D2b phase is marked by a decollement thrust, a system of reverse faults, and gentle folds, associated with SW directed tectonic movements. This deformation is related to an imbricate structure, characteristic of a shallow structural level, and developed in the frontal part of a nappe affecting the Tethyan Zone units of SE Zanskar (Nyimaling-Tsarap Nappe). A later D3 phase generated the Chandra Dextral Shear Zone (CDSZ), a large-scale, ductile, dextral strike-slip shear zone, located in the transition zone between the HHC and the Tethyan Himalaya. The CDSZ most likely represents a part of a system of early Miocene extensional and/or dextral, strike-slip shear zones-observed at the HHC-Tethyan Zone contact along the entire Himalaya. A final D4 phase induced large-scale doming and NE:verging back folding.