Deep incision in an Aptian carbonate succession indicates major sea-level fall in the Cretaceous

Long-term relative sea-level cycles (0 5 to 6 Myr) have yet to be fully understood for the Cretaceous. During the Aptian, in the northern Maestrat Basin (Eastern Iberian Peninsula), fault-controlled subsidence created depositional space, but eustasy governed changes in depositional trends. Relative sea-level history was reconstructed by sequence stratigraphic analysis. Two forced regressive stages of relative sea-level were recognized within three depositional sequences. The first stage is late Early Aptian age (intra Dufrenoyia furcata Zone) and is characterized by foreshore to upper shoreface sedimentary wedges, which occur detached from a highstand carbonate platform, and were deposited above basin marls. The amplitude of relative sea-level drop was in the order of tens of metres, with a duration of <1 Myr. The second stage of relative sea-level fall occurred within the Late Aptian and is recorded by an incised valley that, when restored to its pre-contractional attitude, was >2 km wide and cut 115 m down into the underlying Aptian succession. With the subsequent transgression, the incision was back-filled with peritidal to shallow subtidal deposits. The changes in depositional trends, lithofacies evolution and geometric relation of the stratigraphic units characterized are similar to those observed in coeval rocks within the Maestrat Basin, as well as in other correlative basins elsewhere. The pace and magnitude of the two relative sea-level drops identified fall within the glacio-eustatic domain. In the Maestrat Basin, terrestrial palynological studies provide evidence that the late Early and Late Aptian climate was cooler than the earliest part of the Early Aptian and the Albian Stage, which were characterized by warmer environmental conditions. The outcrops documented here are significant because they preserve the results of Aptian long-term sea-level trends that are often only recognizable on larger scales (i.e. seismic) such as for the Arabian Plate.

Residència universitària Cap Pont de Lleida

Descripció del projecte. S’han de destacar les innovacions i aportacions a l’avanç del coneixement que incorpora el projecte. Es poden incorporar memòries, plànols, fotografies, esbossos, etc. També l’adreça web si s’ha penjat més informació sobre el projecte a la web.DESCRIPCIÓ DE L’EDIFICI: L'edifici s'implanta dintre d'un conjunt d'equipaments universitaris, al àrea de CAP PONT, a Torre Abizando, per la Universitat de Lleida. Està situat en un extrem d'aquest conjunt i recolzant-se sobre l'avinguda Jaume II, a un costat del marge del riu Segre. La forma de l'edifici es per un costat lleugerament corba, adaptant-se a un carrer en pendent, i per l'altra, donant sobre l'interior del campus, la façana es va trencant buscant la millor disposició de vistes, i provocant unes entrades de llum i, vestíbuls, que trenquin el passadís interior de distribució del conjunt d'habitacions que es disposen al llarg del conjunt.

Per què sóc, penso i actuo així (pedagògicamen)t? Influències que han marcat un camí cap a la identitat professional

En aquest article es pretén esbrinar quines són les influències que han portar l"autor a desenvolupar un pensament pedagògic, tant teòricament com pràcticament, des dels inicis com a mestre fins a la pràctica de l"ensenyament a la universitat. Les lectures, la relació amb els companys i amb el context, així com els esdeveniments de la pròpia vida han dut l"autor a desenvolupar una manera de pensar, sentir i actuar en el camp de l"educació. L"article descriu aquest recorregut vital.

Coal deposition in carbonate rich shallow Lacustrine systems: The Calaf and Mequinenza sequences (Oligocene, eastern Ebro Basin, NE Spain)

Two main coal-bearing sequences developed during the Oligocene in the Tertiary Ebro Basin, the Calaf (early Oligocene) and Mequinenza (late Oligocene) coal basins. Coal deposition took place in shallow marsh-swamp-lake complexes which sometimes became closed and evolved under warm climatic conditions with fluctuating humidity. These shallow lacustrine systems are closely interrelated with the terminal parts of the distributive fluvial systems which spread from the tectonically active Ebro basin margins. Laterally extensive lignite-bearing sequences, including rather thin, lenticular autochthonous and/or hypautochthonous coal seams with high ash and sulphur contents, characterized coal deposition in the shallow lacustrine systems. Coal seam geometry, which makes them nearly subeconomic, resulted from the tectonic instability during basin margin evolution and the sometimes closed, arid conditions under which the lacustrine systems evolved. High ash and sulphur contents resulted from the inadequate isolation of peat forming environments from clastic influx and from the very low acidity and sometimes high sulphate contents of the lacustrine waters. Coal exploration in shallow lacustrine sequences similar to those described here must take into account that the spread of coal-forming environments and maxima of coal deposition are usually coincident with lake expansions and retraction or shifting of the terminal fluvial zones interrelated with the lacustrine areas.

Diagenetic processes in a partially dolomitized carbonate reservoir: Casablanca oil field, Valencia Trough, offshore Spain.

Mesozoic and Neogene carbonates located in the Valencia Trough (offshore Spain, western Mediterranean Sea)are oil reservoirs. This paper investigates the diagenetic evolution of the Upper Jurassic limestones, currently dolomitized, that constitute the main reservoir of the Casablanca oil field. Core samples from Casablanca-1A well have been studied to determine the diagenetic products and their relation with porosity evolution, and to reconstruct the fluid flow history prior to and during oil emplacement. On the basis of petrological observations and geochemical analyses (major, minor and trace element composition and oxygen, carbon and strontium isotope composition), a major dolomitization event is recognized postdating subaerial exposure, erosion and karstification. The dolomitization event originated two replacive dolomites (RD1 and RD2) and two dolomite cements (saddle dolomite cement, SDC, and milky-white dolomite cement, MDC)which are partially cogenetic. RD1, RD2 and SDC precipitated at increasing temperatures (over 60ºC and below 110ºC), probably from meteoric water mixed with marine water. The last dolomite type milky-white dolomite cement) precipitated with increasing burial conditions and by arrival of hydrothermal fluids during the Miocene. The post-dolomitization sequence comprises precipitation of calcite cement and partial calcitization of all previous dolomites. The oxygen, carbon and strontium isotope compositions suggest that this calcite cementation occurred from meteoric waters mixed with Burdigalian - Langhian marine waters trapped in the sediments and expelled by compaction in the moderate to deep burial realm. Normal faults were the conduits for upward migration of these fluids as well as for later oil expulsion from the Burdigalian - Langhian source rocks. Late corrosion associated with organic acid-enriched fluids took place prior or simultaneously to oil migration during the Pliocene, enhancing porosity and increasing eservoir quality.

The determinants of CAP reform: learning from the European financial crisis and CAP 2013

There is an ongoing debate on which are the determinants of CAP reform. The economic environment has not been contemplated as a direct determinant of CAP reform but its proxy, the budget, has not only been looked at as such but underlined as a key cause of CAP reform. This paper argues, however, that the budget does not affect the modus operandi of the CAP. It affects the quantity of support each farmer is going to get and sometimes even the timing of the reform, but not the form it is going to receive it. Other CAP determinants and international negotiations in particular, have an impact on the substance of CAP reform. This hypothesis is not contradicted by an analysis of CAP 2013 changes.

Les pintures murals de la basílica paleocristiana de «Es Cap des Port» (Fornells, Menorca): materials i tècniques

[cat]El present treball ofereix una revisió de les pintures murals de la basílica de «Es Cap des Port» (Fornells, Menorca), així com un estudi de caracterització arqueomètrica deIs materials i tècniques per microscòpia òptica, tant amb lupa binocular com amb microscopi petrogràfic mitjançant làmina prima, difracció de raigs X i microscòpia electrònica de rastreig. Els resultats han permès identificar els pigments emprats, així com la seva tècnica d'aplicació. Igualment, han permès caracteritzar els morters i han desvelat l' existència de dos tipus diferents de suport. Malgrat aquestes diferències en els morters, els pigments són sempre els mateixos per a tots els conjunts pictòrics caracteritzats [eng] The present paper offers a revision of the wall paintings found at the early Christian church of 'Es Cap des Port' (Fornells, Menorca). Moreover, the materials and techniques employed have been archaeometrically studied by means of optical microscopy, both with steromicroscope and petrographic microscope by thin section, X-ray diffraction and scanning electron microscopy. The results enable to identify the pigments used, as well as the techniques of application. It has also been possible to characterize the mortars, revealing the existence of two different types of support. In spite of these differences in the mortars, the pigments used are the same ones for all the studied wall paintings

El medi marí del cap de Creus i el golf de Roses

El medi marí de cap de Creus i golf de Roses té unes característiques ecològiques, geològiques i oceanogràfiques excepcionals que han permès el desenvolupament turístic i pesquer de les viles costaneres adjacents, Aquest article sintetitza els principals valors ecològics i econòmics de l'àmbit marí d'aquests dos espais inclosos dins la candidatura de Patrimoni Mundial de la UNESCO

La transformació d'una administració local cap a una administració electrònica sense papers

Aquest treball analitza en què consisteix l'administració electrònica i quines són les adaptacions que ha de realitzar una administració local per transformar-s'hi. El present document també recull quins són els elements clau que cal adaptar dins de l'organització, detallant-los i veient els beneficis d'utilitzar-los. Atès que la inversió econòmica per fer la transformació cap a l'e-Administració pot ser elevada, s'analitzen els serveis que ofereix de forma gratuïta el consorci d'Administració Oberta de Catalunya (AOC), els quals poden ajudar a abaratir la despesa.

Descripció geoambiental i paisatgística del sistema platja-duna de cala Borró (cap Ras, Alt Empordà- Costa Brava, Girona)

The geoambiental and landscape description of the beach-dune system of Cala Borró, (Cap Ras), placed in the town of Colera (Alt Empordà), is carried out. The dunar system, developed with orientation and N-S, links three beach pockets following the topographic slopes of the torrential basins. We find coalescence of dunes in the upper zones, which were possibly an object of reafforestation in the 19thC. to avoid erosion

Cap a una ètica per a la genètica: fonamentació

Voldria iniciar aquest article, plantejant dues qüestions bàsiques: perquè cal preguntar quina ètica per a la genètica, i perquè la genètica requereix d'una tal ètica. Pel que fa a la primera qüestió, quina ètica, cal aclarir que ha de ser una....

Centre d'assitència primària CAP Concòrdia a Sabadell

Award-winning

Apoderament juvenil: com i cap a on?

El treball que es presenta a continuació consisteix en una anàlisi teòrica sobre el concepte d'apoderament juvenil partint d'una aproximació al context actual i les relacions de poder que condicionen la construcció social de la joventut. L'anàlisi es basa en la relació del concepte d'apoderament amb els processos de transformació social així com de qüestionament de les estructures de poder existents avui. D'altra banda, es realitza una reflexió sobre l'ús del terme des de l'àmbit de les ciències socials, específicament des de les polítiques públiques de joventut

Deep incision in an Aptian carbonate succession indicates major sea-level fall in the Cretaceous

Long-term relative sea-level cycles (0 5 to 6 Myr) have yet to be fully understood for the Cretaceous. During the Aptian, in the northern Maestrat Basin (Eastern Iberian Peninsula), fault-controlled subsidence created depositional space, but eustasy governed changes in depositional trends. Relative sea-level history was reconstructed by sequence stratigraphic analysis. Two forced regressive stages of relative sea-level were recognized within three depositional sequences. The first stage is late Early Aptian age (intra Dufrenoyia furcata Zone) and is characterized by foreshore to upper shoreface sedimentary wedges, which occur detached from a highstand carbonate platform, and were deposited above basin marls. The amplitude of relative sea-level drop was in the order of tens of metres, with a duration of <1 Myr. The second stage of relative sea-level fall occurred within the Late Aptian and is recorded by an incised valley that, when restored to its pre-contractional attitude, was >2 km wide and cut 115 m down into the underlying Aptian succession. With the subsequent transgression, the incision was back-filled with peritidal to shallow subtidal deposits. The changes in depositional trends, lithofacies evolution and geometric relation of the stratigraphic units characterized are similar to those observed in coeval rocks within the Maestrat Basin, as well as in other correlative basins elsewhere. The pace and magnitude of the two relative sea-level drops identified fall within the glacio-eustatic domain. In the Maestrat Basin, terrestrial palynological studies provide evidence that the late Early and Late Aptian climate was cooler than the earliest part of the Early Aptian and the Albian Stage, which were characterized by warmer environmental conditions. The outcrops documented here are significant because they preserve the results of Aptian long-term sea-level trends that are often only recognizable on larger scales (i.e. seismic) such as for the Arabian Plate.