Aplicación de criterios geoquímicos al reconocimiento de medios hipersalinos en los materiales arcillosos terciarios de la Depresión Central Catalana

El efecto de distintos ácidos en la puesta en solución de cationes adsorbidos en los minerales de las arcillas ha sido tratado a menudo, tanto desde el punto de vista del estudio de sedimentos arcillosos como del análisis de elementos traza en carbonatos. En este trabajo se estudia el  comportamiento de algunos cationes frente al lavado con agua destilada y con ácido acético (20 % v/v). Asimismo se comparan las concentraciones de cationes en las soluciones de lavado de sedimentos depositados en medios de distinta salinidad. Se observa que, comparando sedimentos de composición mineralógica parecida, las concentraciones de sodio, potasio, litio y magnesio de muestras depositadas en ambientes hipersalinos son mucho más eleva das que las depositadas en ambientes de salinidad menor

Tectonic-palaeoenvironmental forcing of clay-mineral assemblages in nonmarine settings: the Oligocene-Miocene As Pontes Basin (Spain)

Two small, alluvial-lacustrine subbasins developed during the early restraining overstep stages of the Oligocene-Miocene As Pontes strike-slip Basin (NW Spain). Later, the basin evolved into a restraining bend stage and an alluvial-swamp-dominated depositional framework developed. The palaeobiological record demonstrates that the Oligocene-Miocene palaeoclimate in NW Spain was subtropical, warm and humid to subhumid

Depositional models of lacustrine evaporites in the SE margin of the Ebro Basin (Paleogene, NE Spain)

An important evaporitic sedimentation occurred during the Paleogene (Eocene to lower Oligocene) in the Barberà sector of the southeastern margin of the Tertiary Ebro Basin. This sedimentation took place in shallow lacustrine environments and was controlled by a number of factors: 1) the tectonic structuration of the margin; 2) the high calcium sulphate content in the meteoric waters coming from the marginal reliefs; 3) the semiarid climate; and 4) the development of large alluvial fans along the basin margin, which also conditioned the location of the saline lakes. The evaporites are currently composed of secondary gypsum in surface and anhydrite at depth. There are, however, vestiges of the local presence of sodium sulphates. The evaporite units, with individual thicknesses ranging between 50 and 100 m, are intercalated within various lithostratigraphic formations and exhibit a paleogeographical pattern. The units located closer to the basin margin are characterized by a massive gypsum lithofacies (originally, bioturbated gypsum) bearing chert, and also by meganodular gypsum locally (originally, meganodules of anhydrite) in association with red lutites and clastic intercalations (gypsarenites, sandstones and conglomerates). Chert, which is only linked to the thickest gypsum layers, seems to be an early diagenetic, lacustrine product. Cyclicity in these proximal units indicates the progressive development of low-salinity, lacustrine bodies on red mud flats. At the top of some cycles, exposure episodes commonly resulted in dissolution, erosion, and the formation of edaphic features. In contrast, the units located in a more distal position with regard to the basin margin are formed by an alternation of banded-nodular gypsum and laminated gypsum layers in association with grey lutites and few clastic intercalations. These distal units formed in saline lakes with a higher ionic concentration. Exposure episodes in these lakes resulted in the formation of synsedimentary anhydrite and sabkha cycles. In some of these units, however, outer rims characterized by a lithofacies association similar to that of the proximal units occur (nodular gypsum, massive gypsum and chert nodules)

Creació d'una Eina de suport per a la docència en Geoquímica. Una eina d'aprenentatge autònom i d'avaluació

La proposta presentada s'emmarca en un projecte d'innovació docent de la Universitat de Barcelona. L'objectiu és desenvolupar una nova eina interactiva que d'una banda ajudi els alumnes a reforçar i/o ampliar els coneixements de geoquímica de manera autònoma i, de l'altra, sigui un nou recurs d'avaluació per al professorat. Amb el desenvolupament d'aquest eina, l'alumnat disposarà d'un recurs didàctic que li permetrà madurar i ampliar el seus coneixements en el camp de la geoquímica

Els treballs de fi de grau a la Universitat de Barcelona

Podeu consultar la versió castellana al camp recurs relacionat.La implantació dels títols de grau ha suposat un repte per a les universitats, que han hagut d'adaptar els seus projectes formatius a les directrius de l’Espai Europeu d’Educació Superior. Un dels aspectes importants d’aquest procés ha estat l'obligació d’incorporar els treballs de fi de grau (TFG) a l’estructura curricular dels plans d’estudis. Aquesta tasca ha estat complexa i, a més, s’ha vist dificultada per la poca tradició que la majoria de facultats i escoles universitàries tenien en el disseny, l'organització i l'avaluació d’aquest tipus de treball. Uns quants cursos després d’haver-se posat en marxa els TFG, l’Institut de Ciències de l’Educació (ICE) de la Universitat de Barcelona va voler oferir als diferents centres de la UB una plataforma de reflexió i debat on poguessin compartir experiències, plantejar dubtes, analitzar models de bones pràctiques i recollir idees per millorar els seus projectes. A tal efecte, des de la Secció d’Universitat de l’ICE, es va organitzar la jornada «Els treballs de fi de grau a la UB». Aquest quadern recull les comunicacions presentades, sintetitza el debat que van generar i presenta les conclusions a què es va arribar

Los trabajos de fin de grado en la Universidad de Barcelona

Podeu consultar la versió catalana al camp recurs relacionat.[spa] La implantación de los títulos de grado ha supuesto un reto para las universidades, que han tenido que adaptar sus proyectos formativos a las directrices del Espacio Europeo de Educación Superior. Uno de los aspectos importantes de este proceso ha sido la obligación de incorporar los trabajos de fin de grado (TFG) a la estructura curricular de los planes de estudios. Esta tarea ha sido compleja y, además, se ha visto dificultada por la poca tradición que la mayoría de facultades y escuelas universitarias tenían en el diseño, organización y evaluación de esta clase de trabajo. Después de varios cursos de haberse puesto en marcha los TFG, el Instituto de Ciencias de la Educación (ICE) de la Universidad de Barcelona quiso ofrecer a los diferentes centros de la UB una plataforma de reflexión y debate donde pudieran compartir experiencias, plantear dudas, analizar modelos de buenas prácticas y recoger ideas para mejorar sus proyectos. A tal efecto, desde la Sección de Universidad del ICE se organizó la jornada «Los trabajos de fin de grado en la UB». Este cuaderno recoge las comunicaciones presentadas, sintetiza el debate que generaron y presenta las conclusiones a que se llegó.[eng] The phase-in of undergraduate degrees conforming to the guidelines of the European Higher Education Area has been a challenge for universities as far as their training projects are concerned. An important aspect of this process was the need to incorporate the Bachelor’s Degree Final Project (TFG) to the structure of their curricula. This task has been complex and been hampered also by the lack of tradition that most faculties and university colleges had in the design, organization and evaluation of these types of project. Several years after launching the TFG, the Institute of Education Sciences (ICE) of the University of Barcelona (UB) organized the «The Bachelor’s Degree Final Project» conference to offer different centres of the UB a space for reflection and debate to be able to share experiences, ask questions, analyse models of good practices and gather ideas for improving their projects. The present booklet includes papers, summarizes the debate that many and varied contributions generated and outlines the final conclusions reached at this conference

Aplicación de criterios geoquímicos al reconocimiento de medios hipersalinos en los materiales arcillosos terciarios de la Depresión Central Catalana

El efecto de distintos cidos en la puesta en solución de cationes adsorbidos en los minerales de las arcillas ha sido tratado a menudo, tanto desde el punto de vista del estudio de sedimentos arcillosos como del análisis de elementos traza en carbonatos. En este trabajo se estudia el comportamiento de algunos cationes frente al lavado con agua destilada y con ácido actico (20 % v/v). Asimismo se comparan las concentraciones de cationes en las soluciones de lavado de sedimentos depositados en medios de distinta salinidad. Se observa que, comparando sedimentos de composición mineralógica parecida, las concentraciones de sodio, potasio, litio y magnesio de muestras depositadas en ambientes hipersalinos son mucho más elevadas que las depositadas en ambientes de salinidad menor

Aplicación de criterios geoquímicos al reconocimiento de medios hipersalinos en los materiales arcillosos terciarios de la Depresión Central Catalana

El efecto de distintos cidos en la puesta en solución de cationes adsorbidos en los minerales de las arcillas ha sido tratado a menudo, tanto desde el punto de vista del estudio de sedimentos arcillosos como del análisis de elementos traza en carbonatos. En este trabajo se estudia el comportamiento de algunos cationes frente al lavado con agua destilada y con ácido actico (20 % v/v). Asimismo se comparan las concentraciones de cationes en las soluciones de lavado de sedimentos depositados en medios de distinta salinidad. Se observa que, comparando sedimentos de composición mineralógica parecida, las concentraciones de sodio, potasio, litio y magnesio de muestras depositadas en ambientes hipersalinos son mucho más elevadas que las depositadas en ambientes de salinidad menor

Depositional models of lacustrine evaporites in the SE margin of the Ebro Basin (Paleogene, NE Spain)

An important evaporitic sedimentation occurred during the Paleogene (Eocene to lower Oligocene) in the Barberà sector of the southeastern margin of the Tertiary Ebro Basin. This sedimentation took place in shallow lacustrine environments and was controlled by a number of factors: 1) the tectonic structuration of the margin; 2) the high calcium sulphate content in the meteoric waters coming from the marginal reliefs; 3) the semiarid climate; and 4) the development of large alluvial fans along the basin margin, which also conditioned the location of the saline lakes. The evaporites are currently composed of secondary gypsum in surface and anhydrite at depth. There are, however, vestiges of the local presence of sodium sulphates. The evaporite units, with individual thicknesses ranging between 50 and 100 m, are intercalated within various lithostratigraphic formations and exhibit a paleogeographical pattern. The units located closer to the basin margin are characterized by a massive gypsum lithofacies (originally, bioturbated gypsum) bearing chert, and also by meganodular gypsum locally (originally, meganodules of anhydrite) in association with red lutites and clastic intercalations (gypsarenites, sandstones and conglomerates). Chert, which is only linked to the thickest gypsum layers, seems to be an early diagenetic, lacustrine product. Cyclicity in these proximal units indicates the progressive development of low-salinity, lacustrine bodies on red mud flats. At the top of some cycles, exposure episodes commonly resulted in dissolution, erosion, and the formation of edaphic features. In contrast, the units located in a more distal position with regard to the basin margin are formed by an alternation of banded-nodular gypsum and laminated gypsum layers in association with grey lutites and few clastic intercalations. These distal units formed in saline lakes with a higher ionic concentration. Exposure episodes in these lakes resulted in the formation of synsedimentary anhydrite and sabkha cycles. In some of these units, however, outer rims characterized by a lithofacies association similar to that of the proximal units occur (nodular gypsum, massive gypsum and chert nodules)

Depositional models of lacustrine evaporites in the SE margin of the Ebro Basin (Paleogene, NE Spain)

An important evaporitic sedimentation occurred during the Paleogene (Eocene to lower Oligocene) in the Barberà sector of the southeastern margin of the Tertiary Ebro Basin. This sedimentation took place in shallow lacustrine environments and was controlled by a number of factors: 1) the tectonic structuration of the margin; 2) the high calcium sulphate content in the meteoric waters coming from the marginal reliefs; 3) the semiarid climate; and 4) the development of large alluvial fans along the basin margin, which also conditioned the location of the saline lakes. The evaporites are currently composed of secondary gypsum in surface and anhydrite at depth. There are, however, vestiges of the local presence of sodium sulphates. The evaporite units, with individual thicknesses ranging between 50 and 100 m, are intercalated within various lithostratigraphic formations and exhibit a paleogeographical pattern. The units located closer to the basin margin are characterized by a massive gypsum lithofacies (originally, bioturbated gypsum) bearing chert, and also by meganodular gypsum locally (originally, meganodules of anhydrite) in association with red lutites and clastic intercalations (gypsarenites, sandstones and conglomerates). Chert, which is only linked to the thickest gypsum layers, seems to be an early diagenetic, lacustrine product. Cyclicity in these proximal units indicates the progressive development of low-salinity, lacustrine bodies on red mud flats. At the top of some cycles, exposure episodes commonly resulted in dissolution, erosion, and the formation of edaphic features. In contrast, the units located in a more distal position with regard to the basin margin are formed by an alternation of banded-nodular gypsum and laminated gypsum layers in association with grey lutites and few clastic intercalations. These distal units formed in saline lakes with a higher ionic concentration. Exposure episodes in these lakes resulted in the formation of synsedimentary anhydrite and sabkha cycles. In some of these units, however, outer rims characterized by a lithofacies association similar to that of the proximal units occur (nodular gypsum, massive gypsum and chert nodules)