Early Variscan I-type pluton in the pre-Alpine basement of the Western Alps: The ca. 360 Ma Cogne diorite (NW-Italy)

Located at the internal border of the Grand-Saint-Bernard Zone, the diorite and its aureole lie on top of intensively studied Alpine eclogitic units but this pluton, poorly studied yet, has kept locally almost undeformed. The pluton intruded, at similar to 360 Ma, country-rocks mostly composed of dark shales with Na2O > K2O and minor mafic intercalations of tholeiitic basalt affinity. This association is characteristic of the Vanoise (France) basement series, where available age determinations suggest an Early Paleozoic age. Parts of the pluton, and of its hornfels aureole that is evidenced here for the first time, in the Punta Bioula section of Valsavaranche valley (NW-Italy), have been well-preserved from the Alpine deformation. Syn-emplacement hardening, dehydration-induced, probably prevented strain-enhanced Alpine recrystallization. Magmatic rock-types range continuously from subordinate mafic types at SiO2 similar to 48%, of hornblendite with cumulative or appinite affinities, to the main body of quartz diorite to quartz monzonite (SiO2 up to 62%). P-T estimates for the pluton emplacement, based on the abundance of garnet in the hornfelses, using also zircon and apatite saturation thermometry and Al-in-hornblende barometry, suggest T similar to 800-950 degrees C and minimum P in the 0.2-0.5 GPa range, with records of higher pressure conditions (up to 1-2 GPa?) in hornblendite phlogopite-cored amphibole. The high-K, Na > K, calcalkaline geochemistry is in line with a destructive plate-margin setting. Based on major element data and radiogenic isotope signature (epsilon Nd-360 Ma from -1.2 to + 0.9, Sr-87/Sr-86(360 MA) from 0.7054 to 0.7063), the parental magmas are interpreted in terms of deep-seated metabasaltic partial melts with limited contamination from shallower sources, the low radiogenic Nd-content excluding a major contribution from Vanoise tholeiites. There is no other preserved evidence for Variscan magmatism of similar age and composition in the Western Alps, but probable analogs are known in the western and northern parts of French Massif Central. Regarding the Alpine tectonics, not only the age of the pluton and its host-rocks (instead of the Permo-Carboniferous age previously believed), but also its upper mylonitic contact, suggest revisions of the Alpine nappe model. The Cogne diorite allegedly constituted the axial part of the E-verging ``pli en retour [backfold] du Valsavaranche'', a cornerstone of popular Alpine structural models: in fact, the alleged fold limbs, as attested here by field and geochemical data, do not belong to the same unit, and the backfold hypothesis is unfounded. (C) 2012 Elsevier B.V. All rights reserved.

31-11-19 [i.e. 30-11-19], comité du Ice skating club [de Paris] : [photographie de presse] / [Agence Rol]

Référence bibliographique : Rol, 57074

17-12-19, cross country à Antony (interclubs des White Harriers) Redinger, gagnant club Société Générale : [photographie de presse] / [Agence Rol]

Référence bibliographique : Rol, 57170

Combining palaeodistribution modelling and phylogeographical approaches for identifying glacial refugia in Alpine Primula

Aim We investigated the late Quaternary history of two closely related and partly sympatric species of Primula from the south-western European Alps, P. latifolia Lapeyr. and P. marginata Curtis, by combining phylogeographical and palaeodistribution modelling approaches. In particular, we were interested in whether the two approaches were congruent and identified the same glacial refugia. Location South-western European Alps. Methods For the phylogeographical analysis we included 353 individuals from 28 populations of P. marginata and 172 individuals from 15 populations of P. latifolia and used amplified fragment length polymorphisms (AFLPs). For palaeodistribution modelling, species distribution models (SDMs) were based on extant species occurrences and then projected to climate models (CCSM, MIROC) of the Last Glacial Maximum (LGM), approximately 21 ka. Results The locations of the modelled LGM refugia were confirmed by various indices of genetic variation. The refugia of the two species were largely geographically isolated, overlapping only 6% to 11% of the species' total LGM distribution. This overlap decreased when the position of the glacial ice sheet and the differential elevational and edaphic distributions of the two species were considered. Main conclusions The combination of phylogeography and palaeodistribution modelling proved useful in locating putative glacial refugia of two alpine species of Primula. The phylogeographical data allowed us to identify those parts of the modelled LGM refugial area that were likely source areas for recolonization. The use of SDMs predicted LGM refugial areas substantially larger and geographically more divergent than could have been predicted by phylogeographical data alone

Desenvolupament d'una web d'un club esportiu amb entrenaments personalitzats

El propòsit d'aquest projecte és desenvolupar una pàgina web d'un club esportiu que permeti gestionar les parts esportiva, administrativa, i doni a conèixe'l als usuaris d'Internet. Aquesta memòria s'inicia explicant les motivacions, objectius i la planificació del projecte. Seguidament ens situa dins l'estat de l'art en què es troba i s'exposa l'anàlisi de requeriments detallant el que s'espera del producte. Tot seguit, s'explica el modelat de comportament on s'especifiquen els casos d'ús, es presenta el disseny de la BD, les tecnologies utilitzades i una presentació gràfica del portal. Per finalitzar s'exposen els errors trobats amb les solucions pertinents, les proves i les conclusions.

Gondwana-derived microcontinents - The constituents of the Variscan and Alpine collisional orogens

The European Variscan and Alpine mountain chains are collisional orogens, and are built up of pre-Variscan ``building blocks'' which, in most. cases, originated at the Gondwana margin. Such pre-Variscan elements were part of a pre-Ordovician archipelago-like continental ribbon in the former eastern prolongation of Avalonia, and their present-day distribution resulted from juxtaposition through Variscan and/or Alpine tectonic evolution. The well-known nomenclatures applied to these mountain chains are the mirror of Variscan resp. Alpine organization. It is the aim of this paper to present a terminology taking into account their pre-Variscan evolution at the Gondwana margin. They may contain relics of volcanic islands with pieces of Cadomian crust, relics of volcanic arc settings, and accretionary wedges, which were separated from Gondwana by initial stages of Rheic ocean. opening. After a short-lived Ordovician orogenic event and amalgamation of these elements at the Gondwanan margin, the still continuing Gondwana-directed subduction triggered the formation of Ordovician Al-rich granitoids and; the latest Ordovician opening of Palaeo-Tethys. An example from the Alps (External Massifs) illustrates the gradual reworking of Gondwana-derived, pre-Variscan. elements during the Variscan and Alpine/ Tertiary orogenic cycles. (C) 2003 Elsevier Science B.V. All rights reserved.

Interbreedings between Karyotypic Alpine Races of the Common Shrew Sorex-Araneus (Insectivora, Mammalia)

Controlled interbreedings were performed between distinct chromosomal races or forms of Sorex araneus coming from populations of Swiss and French Alps. Four mating pairs including homozygous individuals of the Vaud race, the Valais race, the Intermediate Vaud-Acrocentric form and the Acrocentric form have led to several heterozygous hybrid litters. The karyotypes of the parents were determined from cultures of cartilaginous cells. The karyotypes of the offsprings were determined with a classical method. The production of hybrids between different races suggests the absence of postmating barrier between the Vaud race and the Intermediate form, the Acrocentric form and the Intermediate form, the Acrocentric form and the Valais race.

Determining 241Pu in environmental samples: case studies in alpine soils.

A procedure was developed for determining 241Pu activity in environmental samples. This beta emitter isotope of plutonium was measured by ultra low level liquid scintillation, after several separation and purification steps that involved the use of a highly selective extraction chromatographic resin (Eichrom-TEVA). Due to the lack of reference material for 241Pu, the method was nevertheless validated using four IAEA reference sediments with information values for 241Pu. Next, the method was used to determine the 241Pu activity in alpine soils of Switzerland and France. The 241Pu/239,240Pu and 238Pu/239,240Pu activity ratios confirmed that Pu contamination in the tested alpine soils originated mainly from global fallout from nuclear weapon tests conducted in the fifties and sixties. Estimation of the date of the contamination, using the 241Pu/241Am age-dating method, further confirmed this origin. However, the 241Pu/241Am dating method was limited to samples where Pu-Am fractionation was insignificant. If any, the contribution of the Chernobyl accident is negligible.

Bathonian radiolarians from an ophiolitic melange of the Alpine Tethys (Gets Nappe, Swiss-French Alps)

The determination of radiolarite ages of supraophiolitic rocks date the expansion age of oceanic crust. Radiolarites from the Gets nappe, a decollement cover nappe, provide the means of dating selected localities of outcropping oceanic crust based on their radiolarian faunas. Some studied samples from the ophiolitic melange (Perri re series) have a very well preserved and highly diverse radiolarian fauna of biochronological significance. The age of the radiolarites is established by correlation with the biozonation of Baumgartner et al. (1995b), which indicates a Bathonian age for the oldest radiolarian assemblages. Accordingly, these radiolarites represent remains of the oldest sediments recorded after the opening of the Piemont-Ligurian Ocean. This age is in agreement with those recently established by isotopic methods (166 +/- 1 Ma U-Pb and 165.9 +/- 2.2 Ma Ar-40/Ar-39) in the associated gabbros from the ophiolitic melange. The isotopic age and paleontological results are important because they represent the oldest dating of the oceanic crust of the Piemont-Ligurian Ocean, proving a Late Bajocian-Early Bathonian age for the oceanization in the western Tethys. The systematic part presents a complete Bathonian radiolarian assemblage from two of the best preserved samples; the illustrated assemblage contains 180 species attributed to 66 genera (44 nassellarians, 22 spumellarians and 1 entactinarian). Twenty new species and three new genera (Helvetocapsa, Plicaforacapsa and Theocapsomella) are formally described.

Alpine tectonic evolution of a Jurassic subduction-accretionary complex: Deformation, kinematics and 40Ar/39Ar age constraints on the Mesozoic low-grade schists of the Circum-Rhodope Belt in the eastern Rhodope-Thrace region, Bulgaria-Greece

Deformation of the Circum-Rhodope Belt Mesozoic (Middle Triassic to earliest Lower Cretaceous) low-grade schists underneath an arc-related ophiolitic magmatic suite and associated sedimentary successions in the eastern Rhodope-Thrace region occurred as a two-episode tectonic process: (i) Late Jurassic deformation of arc to margin units resulting from the eastern Rhodope-Evros arc-Rhodope terrane continental margin collision and accretion to that margin, and (ii) Middle Eocene deformation related to the Tertiary crustal extension and final collision resulting in the closure of the Vardar ocean south of the Rhodope terrane. The first deformational event D-1 is expressed by Late Jurassic NW-N vergent fold generations and the main and subsidiary planar-linear structures. Although overprinting, these structural elements depict uniform bulk north-directed thrust kinematics and are geometrically compatible with the increments of progressive deformation that develops in same greenschist-facies metamorphic grade. It followed the Early-Middle Jurassic magmatic evolution of the eastern Rhodope-Evros arc established on the upper plate of the southward subducting Maliac-Meliata oceanic lithosphere that established the Vardar Ocean in a supra-subduction back-arc setting. This first event resulted in the thrust-related tectonic emplacement of the Mesozoic schists in a supra-crustal level onto the Rhodope continental margin. This Late Jurassic-Early Cretaceous tectonic event related to N-vergent Balkan orogeny is well-constrained by geochronological data and traced at a regional-scale within distinct units of the Carpatho-Balkan Belt. Following subduction reversal towards the north whereby the Vardar Ocean was subducted beneath the Rhodope margin by latest Cretaceous times, the low-grade schists aquired a new position in the upper plate, and hence, the Mesozoic schists are lacking the Cretaceous S-directed tectono-metamorphic episode whose effects are widespread in the underlying high-grade basement. The subduction of the remnant Vardar Ocean located behind the colliding arc since the middle Cretaceous was responsible for its ultimate closure, Early Tertiary collision with the Pelagonian block and extension in the region caused the extensional collapse related to the second deformational event D-2. This extensional episode was experienced passively by the Mesozoic schists located in the hanging wall of the extensional detachments in Eocene times. It resulted in NE-SW oriented open folds representing corrugation antiforms of the extensional detachment surfaces, brittle faulting and burial history beneath thick Eocene sediments as indicated by 42.1-39.7 Ma Ar-40/Ar-39 mica plateau ages obtained in the study. The results provide structural constraints for the involvement components of Jurassic paleo-subduction zone in a Late Jurassic arc-continental margin collisional history that contributed to accretion-related crustal growth of the Rhodope terrane. (C) 2011 Elsevier Ltd. All rights reserved.

La Gestió econòmico-empresarial d'un club de futbol

Hi ha records que perduraran sempre; el gol d’Iniesta contra el Chelsea, la boleia de Zidane a Hampden Park… Aquests moments memorables que queden gravats a les retines de tots nosaltres i produeixen una immensa felicitat a l’ésser humà, que l’emocionen, que el fan casi plorar. Tot això es produeix gràcies a un esport de masses molt present en les nostres vides, el futbol. Una activitat merament esportiva que s’ha convertit, amb el pas dels anys, en quelcom més que un esport, ha travessat l’àmbit purament sentimental d’una regió fins a assolir nivells d’autèntica globalització arreu del món. I és precisament el fet que el futbol porta una immensa passió a tots els racons de la societat, el que fa plantejar-nos el funcionament d’aquesta gran indústria de l’entreteniment.La realitat, tanmateix, revela l’existència de tot un món econòmico-empresarial que s’amaga darrere aquest espectacle, del qual, els veritables protagonistes són els clubs de futbol. Sense ells no es produiria mai l’espectacle. És per aquest motiu, que centrarem el nostre anàlisi sobre aquestes entitats esportives: veure el seu funcionament en la seva vessant més econòmica (1).En el present estudi s’analitzarà tot el funcionament intern d’un club, des del seu marc legal fins a l’econòmic, parant molta atenció en el que és el mercat futbolístic, el qual, al cap i a la fi, acaba relacionant la part més esportiva amb l’empresarial. A partir d’aquí intentarem extrapolar aquest entramat al que és el món futbolístic en general.Amb això, intentarem qüestionar-nos el perquè del gran moviment de divises existent, actualment, en aquest esport. Com pot ser que un club inverteixi més de 30 milions d’euros (2) només en el que seria contractar un nou treballador? Com es podengenerar tants recursos per després gastar-los en nòmines astronòmiques pels jugadors?Doncs aquest seguit de qüestions es el que pretenem respondre en aquest treball, de la forma més amena i clara possible, amb els gràfics i taules més adients.(1) Com que de clubs de futbol n’hi ha molts i no els podem analitzar tots un per un, partirem de la based’agafar-ne un com a model, en aquest cas, per la seva proximitat i facilitat d’obtenció de dades hemescollit el FC Barcelona.(2) Quantitat que equival, ni més ni menys, a 500 vegades el sou d’un treballador mitjà al llarg de tota la seva vida

Aerodynamic drag modeling of alpine skiers performing giant slalom turns.

PURPOSE: Aerodynamic drag plays an important role in performance for athletes practicing sports that involve high-velocity motions. In giant slalom, the skier is continuously changing his/her body posture, and this affects the energy dissipated in aerodynamic drag. It is therefore important to quantify this energy to understand the dynamic behavior of the skier. The aims of this study were to model the aerodynamic drag of alpine skiers in giant slalom simulated conditions and to apply these models in a field experiment to estimate energy dissipated through aerodynamic drag. METHODS: The aerodynamic characteristics of 15 recreational male and female skiers were measured in a wind tunnel while holding nine different skiing-specific postures. The drag and the frontal area were recorded simultaneously for each posture. Four generalized and two individualized models of the drag coefficient were built, using different sets of parameters. These models were subsequently applied in a field study designed to compare the aerodynamic energy losses between a dynamic and a compact skiing technique. RESULTS: The generalized models estimated aerodynamic drag with an accuracy of between 11.00% and 14.28%, and the individualized models estimated aerodynamic drag with an accuracy between 4.52% and 5.30%. The individualized model used for the field study showed that using a dynamic technique led to 10% more aerodynamic drag energy loss than using a compact technique. DISCUSSION: The individualized models were capable of discriminating different techniques performed by advanced skiers and seemed more accurate than the generalized models. The models presented here offer a simple yet accurate method to estimate the aerodynamic drag acting upon alpine skiers while rapidly moving through the range of positions typical to turning technique.

Creació d'una discoteca: Amber Club

El món de l’oci nocturn és un món que molta gent disfruta però que ningú acaba de conèixer. Tothom sap per on van els trets principals, però ningú es preocupa profundament per saber realment com funciona, quins són els costos, si els beneficis són elevats, o si és difícil aconseguir que un negoci sigui viable. Aquest, doncs, ha estat el pilar sobre del qual s'ha construït el nostre treball.A través de la creació d’una discoteca i el seu anàlisi cost-benefici hem intentat esbrinar quina és la viabilitat d’un projecte d’aquestes característiques, analitzant tots els costs que s’han d’incórrer, i realitzant un supòsit a la baixa dels ingressos que s’obtindrien.Per dur a terme aquest anàlisi hem realitzat 200 enquestes repartides per les diferents universitats de la província de Barcelona. D’aquesta manera hem pogut analitzar si hi ha demanda per una nova discoteca i quines són les preferències del consumidor.Una vegada fet aquest anàlisi, hem procedit a la recerca d'un local que s'adapti a les nostres necessitats i a les mostrades pel públic enquestat. Al no voler entretenir-nos en qüestions com la decoració del local, o l’adaptació d’aquest a tota la normativa vigent, hem partit del supòsit que un local que actualment funciona estigués disponible pel lloguer, concretament Opium Mar. Hem introduït un seguit de reformes que creiem necessàries pel millor funcionament, i a continuació hem començat amb les estratègies de màrqueting i la determinació dels serveis oferts.Dos punts seran claus per tal que la discoteca funcioni correctament. Primer de tot, el fet que sigui coneguda per un gran públic, i llavors que aquest públic en qüestió estigui content amb el serveis oferts. És per això que hem destinat un gran nombre de recursos en màrqueting (pàgina web, mailing , SMS...) i ens hem centrat també amb tots els serveis que podem oferir (guarda-roba, sales VIP...). La reputació, ens han dit molts responsables, pot ser l’eina que pot fer del teu projecte una gran font d’ingressos, o el contrari, una gran pèrdua de diners.També ens hem centrat en el personal i el subministrament de begudes, calculant així quin és el nombre de treballadors necessaris per tirar endavant el projecte, i quin és l’estoc de begudes òptim que hem de tenir per cobrir tota la demanda.Finalment, hem tingut en compte els impostos que hem d'incórrer a un projecte d'aquest tipus, ja sigui impost de societats, el cost de la llicència per exercir l'activitat, IVA, etc.Una conclusió és clara després de la realització d’aquest projecte: la nostra discoteca és rendible, i per extensió qualsevol altre amb un nombre considerable d’assistència. El valor afegit que crea un projecte d’aquestes magnituds és tan gran, i la despesa mitjana de la gent en oci nocturn tan considerable, que un projecte capaç de portar un nombre de clients relativament petit en funció del local, pot presentar beneficis