Expressão geofísica-estrutural do lineamento transbrasiliano na porção central da Bacia do Parnaíba (Maranhão-Piauí)

The objective of this study was to characterize the structural-geophysical expression of the Transbrasiliano Lineament (TBL) in the east-central portion of the Parnaíba Basin. The TBL corresponds to a major Neoproterozoic NE-trending shear zone related to the Brasiliano orogenic cycle, with dextral strike-slip kinematics, underlying (but also laterally exposed in the NE and SW basin edges) the sedimentary section of the Parnaíba Basin. In this study, the interpretation of gravity and magnetic anomaly maps is consistent with the TBL kinematics, the signature of the geophysical anomalies corresponding to the high (plastic behaviour) and subsequent declining temperature (ductile to brittle behaviour) stages during Brasiliano and late Brasiliano times. The pattern of residual gravity anomalies is compatible with an S-C dextral pair shaping the geological bodies of an heterogeneous basement, such as slices of gneisses and granulites (positive anomalies), granitic and low-medium grade metasedimentary rocks (negative anomalies). Such anomalies curvilinear trends, ranging from NNE (interpreted as S surfaces) to NE (C surfaces), correspond to flattening surfaces (S), while the NE rectilinear trend must represent a C band. The narrower magnetic anomalies also display NNE to NE (S surfaces) trends and should correspond to similar (although narrower and more discontinuous) sources in the equivalent anomaly patterns. Pre-Silurian pull-apart style grabens may contribute to the NE negative gravimetric anomalies, although this interpretation demands control by seismic data analysis. On the other hand, the curvilinear anomalies associated to contractional trends are incompatible with their interpretation as pre-Silurian graben, in both maps. In the (reduced to the pole) magnetic anomalies map, most of these are again associated to low-temperature shear zones (C planes) and faults, juxtaposing distinct blocks in terms of magnetic properties, or eventually filled with basic bodies. It is also possible that some isolated magnetic anomalies correspond to igneous bodies of late-Brasiliano or Mesozoic age. The basement late discontinuities pattern can be interpreted in analogy to the Riedel fractures model, with steep dipping surfaces and a sub-horizontal movement section. This study also explored 2D gravity modeling controlled by the interpretation of a dip seismic line as regards to the Transbrasiliano Lineament. The rock section equivalent to the Jaibaras Group occupying a graben structure (as identified in the seismic line) corresponds to a discrete negative anomaly superimposed to a gravimetric high, once again indicating a stronger influence of older crystalline basement rocks as gravimetric sources, mainly reflecting the heterogeneities and anisotropies generated at high temperature conditions and their subsequent cooling along the TBL, during the Brasiliano cycle.

Expressão geofísica-estrutural do lineamento transbrasiliano na porção central da Bacia do Parnaíba (Maranhão-Piauí)

The objective of this study was to characterize the structural-geophysical expression of the Transbrasiliano Lineament (TBL) in the east-central portion of the Parnaíba Basin. The TBL corresponds to a major Neoproterozoic NE-trending shear zone related to the Brasiliano orogenic cycle, with dextral strike-slip kinematics, underlying (but also laterally exposed in the NE and SW basin edges) the sedimentary section of the Parnaíba Basin. In this study, the interpretation of gravity and magnetic anomaly maps is consistent with the TBL kinematics, the signature of the geophysical anomalies corresponding to the high (plastic behaviour) and subsequent declining temperature (ductile to brittle behaviour) stages during Brasiliano and late Brasiliano times. The pattern of residual gravity anomalies is compatible with an S-C dextral pair shaping the geological bodies of an heterogeneous basement, such as slices of gneisses and granulites (positive anomalies), granitic and low-medium grade metasedimentary rocks (negative anomalies). Such anomalies curvilinear trends, ranging from NNE (interpreted as S surfaces) to NE (C surfaces), correspond to flattening surfaces (S), while the NE rectilinear trend must represent a C band. The narrower magnetic anomalies also display NNE to NE (S surfaces) trends and should correspond to similar (although narrower and more discontinuous) sources in the equivalent anomaly patterns. Pre-Silurian pull-apart style grabens may contribute to the NE negative gravimetric anomalies, although this interpretation demands control by seismic data analysis. On the other hand, the curvilinear anomalies associated to contractional trends are incompatible with their interpretation as pre-Silurian graben, in both maps. In the (reduced to the pole) magnetic anomalies map, most of these are again associated to low-temperature shear zones (C planes) and faults, juxtaposing distinct blocks in terms of magnetic properties, or eventually filled with basic bodies. It is also possible that some isolated magnetic anomalies correspond to igneous bodies of late-Brasiliano or Mesozoic age. The basement late discontinuities pattern can be interpreted in analogy to the Riedel fractures model, with steep dipping surfaces and a sub-horizontal movement section. This study also explored 2D gravity modeling controlled by the interpretation of a dip seismic line as regards to the Transbrasiliano Lineament. The rock section equivalent to the Jaibaras Group occupying a graben structure (as identified in the seismic line) corresponds to a discrete negative anomaly superimposed to a gravimetric high, once again indicating a stronger influence of older crystalline basement rocks as gravimetric sources, mainly reflecting the heterogeneities and anisotropies generated at high temperature conditions and their subsequent cooling along the TBL, during the Brasiliano cycle.

I terremoti storici hanno fatto più danni nella parte nord-occidentale di Bologna: ricerca di una spiegazione geofisica per questo fenomeno

Dallo studio della sismicità storica della città di Bologna (Guidoboni e Boschi, 2003) emerge che la maggior parte dei danni causati dai terremoti è concentrata nella parte Nord e Nord-Ovest della città, a nord delle attuali vie S. Donato e S. Isaia. In questo lavoro abbiamo studiato la risposta sismica in diversi siti del centro storico di Bologna, per capirne il comportamento in caso di terremoto e verificare se i risultati fossero compatibili con i dati storici. È stata effettuata una campagna di misure geofisiche: 52 con tecnica passiva a stazione singola HVSR per misurare le frequenze di amplificazione dei sottosuoli (47 all’interno delle mura), 5 in array per misurare l’andamento delle velocità delle onde di taglio nel sottosuolo (tutte all’interno delle mura). 22 delle 47 misure H/V mostrano amplificazione nell’intervallo di frequenze tra 1 e 10 Hz, quello di interesse per le strutture del centro storico. Le cause di queste amplificazioni si ipotizzano essere un livello ghiaioso a circa 10-15 m di profondità (Fiori, 2002) in approfondimento da centro città verso est, e un livello sabbioso a circa 10 m di profondità (Amorosi, 2014). Le misure in array, invece, indicano sostanzialmente che l’estremità orientale della città storica ha rigidezze maggiori a profondità maggiori di 50 m. Il dato derivante dalla sismologia storica, in sintesi, non pare essere completamente supportato da evidenze geologiche o geofisiche: la risposta sismica all’interno delle mura di Bologna varia leggermente da punto a punto, ma senza mostrare trend applicabili ad estese macroaree. Solo l’estremo Nord-Est della città ha un comportamento amplificativo più omogeneo (amplificazione a 1-3 Hz) in linea con la geologia locale, che presenta livelli marcatamente ghiaiosi sotto i 15 m di profondità. La variabilità geologica e di risposta sismica locale è stata verificata essere molto maggiore fuori dalle mura di cinta della città.

Co-simulación HW/SW en Raspberry Pi

En el mundo de la simulación existen varios tipos de sistemas reales, entre los que se encuentran los sistemas de eventos discretos. Para poder simular estos sistemas se pueden utilizar, entre otras, herramientas basadas en el formalismo DEVS (Discrete EVents system Specification), como la utilizada en este proyecto: xDEVS. La simulación posee una importancia muy elevada en campos como la educación y la ciencia, y en ocasiones es necesario incluir datos del medio físico o sacar información al exterior del simulador. Por ello es necesario contar con herramientas que puedan realizar simulaciones utilizando sensores, actuadores, circuitos externos, etc., o lo que es lo mismo, que puedan realizar co-simulaciones entre software y hardware. De esta forma se puede facilitar el desarrollo de sistemas por medio de modelado y simulación, pudiendo extraer el hardware gradualmente y analizar los resultados en cada etapa. Este proyecto es de carácter incremental, y trata de extender la funcionalidad de la plataforma xDEVS para poder realizar co-simulaciones entre hardware y software sobre una Raspberry Pi. Para ello se van a utilizar circuitos lógicos como hardware externo y se enlazarán al simulador a través de ficheros de dispositivo, gestionados por módulos del kernel de Linux. Como caso de estudio se desarrolla la co-simulación entre hardware y software completa de un ascensor de siete plantas para mostrar el uso y funcionamiento en xDEVS, extrayendo los circuitos integrados de uno en uno.

L'activation de la PI 3-kinase par les récepteurs [bêta]-adrénergiques est dépendante du sous-type

Mémoire numérisé par la Direction des bibliothèques de l'Université de Montréal.

L'activation de la PI 3-kinase par les récepteurs [bêta]-adrénergiques est dépendante du sous-type

Mémoire numérisé par la Direction des bibliothèques de l'Université de Montréal.

Two devices, each of which measure water velocity; on the right is an acoustic device that is permanently maintained at Gumbo Limbo by PI Rene Price; on the left is a 3D camera with a long fiberoptic lens, deployed for testing purposes by collaborator Evan Variano.

http://digitalcommons.fiu.edu/fce_lter_photos/1303/thumbnail.jpg

Assistant Professor and FCE Co-PI, John Kominoski and collaborators, Chris McVoy and Jim Brock, are investigating the foundational role of floc in the structural and functional attributes of the ridge and slough ecosystems of the Central Everglades.

http://digitalcommons.fiu.edu/fce_lter_photos/1336/thumbnail.jpg

Aplicação do método de Monte Carlo no estudo da padronização de radionuclídeos com esquema de desintegração complexos em sistema de coincidencias 4-pi-beta-gama

Tese (Doutoramento)

Desenvolvimento de um sistema eletronico com registro simultaneo de amplitude e instante de ocorrencias dos pulsos, aplicado ao metodo de coincidencias 4'pi''beta''gama'

Dissertacao (Mestrado)

Che vinca il più Forte. Proposta di traduzione, analisi e commento di "Wojna polsko-ruska pod flagą biało-czerwoną" di Dorota Masłowska.

Traduzione dal polacco in italiano - accompagnata da analisi e commento dei temi proposti - di alcuni estratti dal bestseller della scrittrice polacca adolescente, che racconta il mondo visto dagli occhi di un giovane disoccupato poco istruito di provincia. Un'immagine cruda e senza filtri della gioventù in Polonia negli anni di transizione dalla caduta del muro di Berlino all'ingresso nell'Unione Europea. Un momento storico impossibile da collocare nella ripetitività tipica dei grandi avvenimenti in Polonia, vissuto direttamente sulla pelle dei suoi protagonisti, cioè i giovani senza né passato né futuro, incapaci di coltivare il presente.

Évaluation de modèles prévisionnels de la fusariose de l'épi chez le blé sous les conditions de culture du Québec

La fusariose de l’épi est une maladie fongique des cultures céréalières au Québec. Les objectifs de ce projet étaient de vérifier l’influence de quatre facteurs (météorologie, cultivar, date de semis, fongicide) sur les rendements et la qualité du blé et d’évaluer les performances de neuf modèles à prédire l’incidence de cette maladie. Pendant deux ans, à quatre sites expérimentaux au Québec, des essais de blé de printemps et d’automne ont été implantés pour amasser un jeu de données météorologiques, phénologiques et épidémiologiques. L’application d’un fongicide a réduit la teneur en désoxynivalénol des grains dans neuf essais sur douze et a augmenté les rendements dans sept essais. De plus, les modèles prévisionnels américains et argentins ont eu de meilleures performances que les modèles canadiens et italiens quand leur seuil de décision était ajusté et que le développement du blé était suivi au champ.

Master in Innovative Tourism Development: a blended learning experience in the Polytechnic Institute of Viana do Castelo

This chapter analyses a Portuguese HEI’s first experience with blended learning. Focusing on the Master in Innovative Tourism Development currently being held at the Superior School of Technology and Management of the Polytechnic Institute of Viana do Castelo, it presents the institutional background and rationale behind the course’s implementation, identifying its strengths and weaknesses, as well as areas of potential development. Based on an evaluation research carried out throughout the course’s first three editions and that involved students, faculty and institutional leaders, it summarizes the main results of a long term-study, putting forth a set of recommendations for improvements and defining potential areas of intervention in future editions of the course.