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Salito d’a imprenta o día 4 de chunio de 2010 –seguntes se siñala en a zaguera plana– e presentato ixe mesmo día en o Instituto de Estudios Altoaragoneses como auto prebio á ra inaugurazión d’a 27ena Feria d’o Libro de Uesca, que se ferba ixa mesma tardada, o libro replega, en transcrizión feita por Mª. Dolores Barrios Martínez, decumentos d’a colechiata de Santa María d’Alquezra de os sieglos XI, XII e XIII...

A pesar de haberse introducido hace casi dos décadas en la escuela primaria, hasta nuestros días apenas se han desarrollado trabajos de investigación centrados en la situación y perspectivas de futuro de la lengua aragonesa dentro del ámbito educativo. Con el fin de aportar las primeras claves a este respecto, estamos desarrollando un amplio estudio de naturaleza multimetodológica centrado principalmente en el análisis de las actitudes lingüísticas de la comunidad educativa, el cual abarca al profesorado, equipos directivos, familias y alumnado de las escuelas públicas altoaragonesas, así como a los maestros en formación en la Universidad de Zaragoza.

As denominazions populars d’a chen d’os lugars de l’Alto Aragón (e d’Aragón en cheneral) son en muitos casos descriptibas e de gran poder d’ebocazión, tanto por l’azión que reflexan, como por a suya sonoridá, e en bel caso por a suya rima con o toponimo a que fan referenzia. Muitas d’as denominazions son palabras compuestas en aragonés: creyemos que ye intresán fer una relazión e un analís d’istas como contrebuzión á o estudio d’a formazión de palabras en aragonés, en concreto d’os prozedimientos de composizión. Ta fer o treballo rancamos d’o corpus que replega Andolz (1992: 633-641; 1996). Consideramos solamén a composizión, no pas a deribazión. Nos limitamos prenzipalmén á os lugars de l’Alto Aragón, ye dizir, d’o territorio propio de l’aragonés; con tot e con ixo, aprobeitamos tamién bellas formazions intresans que se rechistran en lugars de territorios de fabla catalana u de territorios d’Aragón d’o zentro e d’o sur, castellanizatos fa tiempos. Las denominaciones populares de la gente de los pueblos del Alto Aragón (y de Aragón en general) son en muchos casos descriptivas y de gran poder de evocación. Muchas de ellas son palabras compuestas en aragonés. En este trabajo las recopilamos y analizamos, como contribución al estudio de la formación de palabras en aragonés, en concreto de los procedimientos de composición.

Analisi des discorsi sus era identitat aranesa en Internet pendent era polemica pera aprobacion deth Projècte de Lei de Vegueries, en hereuèr de 2010. A trauès der estudi d'aguesti discorsi s'identifiquen quini son es principaus trèits identitaris damb es quaus se definissen es aranesi., Anàlisi dels discursos sobre la identitat aranesa a Internet durant la polèmica per l'aprovació del Projecte de Llei de Vegueries, el mes de febrer de 2010. A través de l'estudi d'aquests discursos s'identifiquen quins són els principals trets identitaris amb els quals es defineixen els aranesos., Análisis de los discursos sobre la identidad aranesa en Internet durante la polémica por la aprobación del Proyecto de Ley de Veguerías, el mes de febrero de 2010. A través del estudio de estos discursos se identifican cuáles son los principales rasgos identitarios con los que se definen los araneses., This paper analyses the discourses on Aranese identity on the Internet throughout the controversy over the adoption of the Vegueries Law, on February 2010. Through the study of these discourses are identified the main identitary traits with which Aranese define themselves.

The clone, especially in its audiovisual version, has often been treated as a marginalized being and its body understood as a repository of violence and pain, especially since its mere existence has traditionally been subjected to maintaining the integrity of the ‘original’ human body. This is visible in films in which we observe the figure of the clone treated in ways contrary to the critical posthumanism postulated by Braidotti, Ferrando or Vint, among others. The Island (2005), Never Let me Go (2010) or the animated series World of Tomorrow (2015, 2017, 2020) make us reflect on our responsibility toward the consequences of certain uses of biomechanical technology. A process of social denunciation is carried out through the emphasis that these films give to posthuman subjectivity, and thus these clones show their concerns and make viewers participants in their marginalized experience. Viewers see life from their perspective, we share their biological consciousness and their very existence leads us to reflection and denunciation

The Sanabria appinitic rocks and host migmatites form an unusual, non-peri-batholithic complex in which all the typical members of the appinite suite are present. It differs from most appinitic complexes in the deeper level of emplacement and the close temporal and spatial association with migmatites. Consequently, many in situ relationships that resulted from the invasion of mafic magma into a crustal anatectic zone are extremely well preserved. The complex shows unequivocal relations between members of the appinitic suite and between these and migmatites derived by anatexis of a gneissic formation (Ollo de Sapo gneiss). These relations point to derivation of monzodiorites and biotite diorites by hydrous basalt fractionation combined with fluid-assisted melting of the crustal rocks surrounding the appinitic intrusions. This hydrous basic magma may be derived from an enriched region of the mantle associated with subduction. Petrogenetic models have been tested using a combination of field relations and geochemical data. Despite the complexity of the processes involved, it is concluded that water played an important role in the petrogenesis of the intermediate and mafic magmas. Reaction between monzodiorite melts and the host migmatites was responsible for the generation of a range of intermediate rocks within the complex. The need for water to facilitate magma generation in both the mantle and the crust suggests that melting is linked with subduction. This interpretation has important implications because appinitic magmatism may be considered as indicative of subduction processes involved not only in the generation of the mafic end-members of the suite, but also in the generation of batholiths with which the appinitic rocks are spatially and temporally associated.

The stratigraphic basis of this work has allowed the use of larger foraminifers in the biostratigraphic characterisation of the new Shallow Benthic Zones (SBZ). This part of the volume presents a description of the sedimentary cycles formed by the transgressive-regressive systems of the Lutetian and Bartonian in the southeastern sector of the Ebro Foreland Basin. Concerning the Lutetian deposits studied in the Amer-Vic and Empordà areas, four sedimentary cycles have been characterised. The first and second are found within the Tavertet/Girona Limestone Formation (Reguant, 1967; Pallí, 1972), while the third and fourth cycles cover the Coll de Malla Marl Formation (Clavell et al., 1970), the Bracons Formation (Gich, 1969, 1972), the Banyoles Marl Formation (Almela and Ríos, 1943), and the Bellmunt Formation (Gich, 1969, 1972). In the Bartonian deposits studied in the Igualada area, two transgressive-regressive sedimentary cycles have been characterised in the Collbàs Formation (Ferrer, 1971), the Igualada Formation (Ferrer, 1971), and the Tossa Formation (Ferrer, 1971). The Shallow Benthic Zones (SBZs) recognised within the Lutetian are the following: SBZ 13, from the Early Lutetian, in the transgressive system of the first cycle; SBZ 14, from the Middle Lutetian, in the second cycle and the lower part of the transgressive system of the third cycle; SBZ 15, from the Middle Lutetian, in the remaining parts of the third system; SBZ 16, from the Late Lutetian, throughout the fourth cycle. The association of larger foraminifers in the first and second cycles of the Bartonian in the Igualada area has been used as the basis for the definition of SBZs 17 and 18 recognised in the Bartonian of the western Tethys.

The elastic scattering and inclusive α-particle yield for the 6He + 206Pb system at an incident energy of 18 MeV, just below the nominal Coulomb barrier, have been measured. The α-particle yield at forward angles is also reported. The data are analyzed by means of continuum-discretized coupled-channels, distorted wave Born approximation, and coupled reaction channels calculations. Couplings to the one-neutron- and two-neutron-transfer reactions are found to be able to account for most of the absorption in the entrance channel., This work was supported in part by Grant No. FPA2010-22131-C02-01 from the Spanish Ministry of Science.

We analyse here a wide sample of carbonaceous chondrites from historic falls (e.g. Allende, Cold Bokkeveld, Kainsaz, Leoville, Murchison, Murray, Orgueil and Tagish Lake) and from NASA Antarctic collection. With the analysis of these meteorites we want to get new clues on the role of aqueous alteration in promoting the reflectance spectra diversity evidenced in the most primitive chondrite groups. The selected meteorite specimens are a sample large enough to exemplify how laboratory reflectance spectra of rare groups of carbonaceous chondrites exhibit distinctive features that can be used to remotely characterize the spectra of primitive asteroids. Our spectra cover the full electromagnetic spectrum from 0.2 to 25 μm by using two spectrometers. First one is an ultraviolet (UV)–near-infrared (NIR) spectrometer that covers the 0.2–2 μm window, while the second one is an attenuated total reflectance infrared spectrometer covering the 2–25 μm window. In particular, laboratory analyses in the UV–NIR window allow obtaining absolute reflectance by using standardized measurement procedures. We obtained reflectance spectra of specimens belonging to the CI, CM, CV, CR, CO, CK, CH, R and CB groups of carbonaceous chondrites plus some ungrouped ones, and it allows identifying characteristic features and bands for each class, plus getting clues on the influence of parent body aqueous alteration. These laboratory spectra can be compared with the remote spectra of asteroids, but the effects of terrestrial alteration forming (oxy)hydroxides need to be considered., Current research was supported by the Spanish Ministry of Science and Innovation (project: AYA2011-26522) and CSIC (starting grant #201050I043). JL1 is grateful to ICREA Academia program. ZM acknowledges support from the Royal Society. NASA Meteorite Working Group and Johnson Space Center meteorite curators are acknowledged for providing the Antarctic carbonaceous chondrites. We also want to express our sincere gratitude for the valuable effort made over the years in the recovery of Antartic samples by ANSMET (The Antarctic Search for Meteorites programme). Katsuhito Othsuka and R. H. are also acknowledged for providing some of the carbonaceous chondrites from historic falls.