1000 resultados para Pagès, Jaume -- Intervius


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The El Soplao site is a recently-discovered Early Albian locality of the Basque-Cantabrian Basin (northern Spain) that has yielded a number of amber pieces with abundant bioinclusions. The amber-bearing deposit occurs in a non-marine to transitional marine siliciclastic unit (Las Peñosas Formation) that is interleaved within a regressive-transgressive, carbonate-dominated Lower Aptian-Upper Albian marine sequence. The Las Peñosas Formation corresponds to the regressive stage of this sequence and in its turn it splits into two smaller regressive-transgressive cycles. The coal and amber-bearing deposits occur in deltaic-estuarine environments developed during the maximum regressive episodes of these smaller regressive-transgressive cycles. The El Soplao amber shows Fourier Transform Infrared Spectroscopy spectra similar to other Spanish Cretaceous ambers and it is characterized by the profusion of sub-aerial, stalactite-like flows. Well-preserved plant cuticles assigned to the conifer genera Frenelopsis and Mirovia are abundant in the beds associated with amber. Leaves of the ginkgoalean genera Nehvizdya and Pseudotorellia also occur occasionally. Bioinclusions mainly consist of fossil insects of the orders Blattaria, Hemiptera, Thysanoptera, Raphidioptera, Neuroptera, Coleoptera, Hymenoptera and Diptera, although some spiders and spider webs have been observed as well. Some insects belong to groups scarce in the fossil record, such as a new morphotype of the wasp Archaeromma (of the family Mymarommatidae) and the biting midge Lebanoculicoides (of the monogeneric subfamily Lebanoculicoidinae). This new amber locality constitutes a very significant finding that will contribute to improving the knowledge and comprehension of the Albian non-marine paleoarthropod fauna.

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Un muestreo intensivo del clasico yacimiento de mamíferos fósles de Santpedor ha dado como resultado la presencia de Theridomys aff. aquatilis, Gliravus aff. priscus, Eucricetodon atavus y Pseudoltinomys gaillardi. Esta asociacin permite atribuir 1os niveles del yacimiento al Oligoceno inferior mas bajo (nivel de Hoogbutsel)

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Relaciones entre las asociaciones de facies de las tres unidades litoestratigráficas del complejo turbidítico y su asimilación a unidades deposicionales dentro de modelos de sedimentación submarina.

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Se señala la presencia de caliche fósil en el Triásico inferior y el cual es interpretado como caliche inicialmente maduro producido en cortas exposiciones subáreas en condiciones semiáridas. Se deducen das tipos de ambientes de acuerdo con los dos modelos $e secuencias litolgicas en las que se encuentra el caliche: partes distale de glacis de acumulación y 'playas', y diques y charcas en una llanura aluvial meandriforme.

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The decapod burrow Spongeliomorpha sudolica occurs associated with transgressive firmgrounds in the transition between Aragonian continental red beds and Langhian marine units in some of the inner sectors of the Vallès-Penedès Basin. This ichnospecies designates branching burrow systems with scratch marks in the walls produced by marine crustacean decapods. The occurrence of Spongeliomorpha represents an example of theGlossifungites ichnofacies. The several horizons where the traces are found are intercalated with continental red beds a few meters below the main transgressive surface, which is overlain by fossiliferous marine sandstones. The Spongeliomorpha-bioturbated layers record short, high frequency marine flooding surfaces that may be related either to actual sea-level changes or to variations in tectonic subsidence or sediment input. In any case, these flooding events punctuated the early phases of the Langhian transgression in the basin.

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La unidad de limos intermedios del delta del Llobregat corresponde a un ambiente prodeltaico en el que se han identificado, por comparación al modelo actual, subambientes de prodelta proximal, medio y medio-distal. Su agua intersticial es sinsedimentaria, hallándose en la actualidad parcialmente diluida.

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El relleno sedimentari de edad Priaboniense superior-Chattiense dcl sector oriental de la cuencade antepaís del Ebro puede subdividirse en cinco secuencias deposicionales, definidas en base a 1os principales cambios paleogeográficos que afectaron alos sistemas aluviales y lacustres en la región. Tanto el desarrollo de estructuras tectónicas superficiales como 1os procesos de ajuste isostático regional son considerados como 1os principales factores de control de esta evolución sedimentaria. Los cinco sistemas lacustres reconocidos (La Noguera, L'Anoia, Segarra, L'Urgell y Los Monegros) muestran unas caracteristicas de extensión areal y desarrollo de facies fuertemente controladas por su situación respecto a las zonas de máxima subsidencia. Las tendencias megasecuenciales de cambio o de alternancia de deposición evaporítica y carbonatada, son atribuidas aquí tanto a posibles cambios climáticos como a cambios en la composición del área fuente. Estos fueron inducidos por la evolución tectónica de los margenes de la cuenca.

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La evolución de los sistemas lacustres cenozoicos en España estuvo claramente influida por: l) la edificación de los orógenos pirenaico y bético y la intensa deformación interna que afectó la microplaca de Iberia. 2) l0s cambios de las condiciones paleogeogrlficas y paleoclimáticas generales que afectaron la región mediterránea occidental-atlántica oriental en la que se localizaba Iberia. Potentes sucesiones de carbonatos y evaporitas lacustres han sido reconocidas en la mayor parte de las cuencas cenozoicas españolas. Junto a estos depósitos se registra la presencia de otros menos frecuentes (carbón, devósitos bituminosos, diatomitas, arcillas especiales) también significativos desde un punto de vista geolimnolÓgico e interesantes desde una perspectiva económica. Los mayores y mis persistentes sistemas lacustres se ubicaron en las cuencas de antepaís, arealmente muy extensas. Los de menor entidad y mis corta evolución se formaron en cuencas limitadas por fallas de distintos tipos. En ambos casos los sistemas lacustres evolucionaron en estrecharelacióncon sistemas aiuviales y sus características hidroquírnicas estuvieron muy influidas por el reciclaje de depósitos de carbonatos, sulfatos y cloruros, fundamentalmente de edad mesozoica. Este reciclaje influyó tanto en la litologia de las sucesiones lacustres resultantes como sobre las caracteristicas de las asociaciones de organismos limnicos que se desarrollaron en los sistemas lacustres.

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We consider a general class of non-Markovian processes defined by stochastic differential equations with Ornstein-Uhlenbeck noise. We present a general formalism to evaluate relaxation times associated with correlation functions in the steady state. This formalism is a generalization of a previous approach for Markovian processes. The theoretical results are shown to be in satisfactory agreement both with experimental data for a cubic bistable system and also with a computer simulation of the Stratonovich model. We comment on the dynamical role of the non-Markovianicity in different situations.

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The turn-on process of a multimode VCSEL is investigated from a statistical point of view. Special attention is paid to quantities such as time jitter and bit error rate. The single-mode performance of VCSEL¿s during current modulation is compared to that of edge-emitting lasers.

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Characteristic decay times for relaxation close to the marginal point of optical bistability are studied. A model-independent formula for the decay time is given which interpolates between Kramers time for activated decay and a deterministic relaxation time. This formula gives the decay time as a universal scaling function of the parameter which measures deviation from marginality. The standard deviation of the first-passage-time distribution is found to vary linearly with the decay time, close to marginality, with a slope independent of the noise intensity. Our results are substantiated by numerical simulations and their experimental relevance is pointed out.

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We develop a singular perturbation approach to the problem of the calculation of a characteristic time (the nonlinear relaxation time) for non-Markovian processes driven by Gaussian colored noise with small correlation time. Transient and initial preparation effects are discussed and explicit results for prototype situations are obtained. New effects on the relaxation of unstable states are predicted. The approach is compared with previous techniques.

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The frequency dynamics of gain-switched singlemode semiconductor lasers subject to optical injection is investigated. The requirements for low time jitter and reduced frequency chirp operation are studied as a function of the frequency mismatch between the master and slave lasers. Suppression of the power overshoot, typical during gain-switched operation, can be achieved for selected frequency detunings.

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The propagator of a relativistic spinning particle is calculated using the Becchi-Rouet-Stora-Tyutin-(BRST)-invariant path-integral formalism of Fradkin and Vilkovisky. The spinless case is considered as an introduction to the formalism.

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The general theory of nonlinear relaxation times is developed for the case of Gaussian colored noise. General expressions are obtained and applied to the study of the characteristic decay time of unstable states in different situations, including white and colored noise, with emphasis on the distributed initial conditions. Universal effects of the coupling between colored noise and random initial conditions are predicted.