1,206 research outputs found

    La ciudadanĂ­a europea como presupuesto de la Carta de derechos fundamentales.

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    Gluon propagator, triple gluon vertex and the QCD coupling constant

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    We study the UV-scaling of the flavorless gluon propagator in the Landau gauge in an energy window up to 9 GeV. Dominant hypercubic lattice artifacts are eliminated. A large set of renormalization schemes is used to test asymptotic scaling. We compare with our results obtained directly from the triple gluon vertex. We end-up with \Lambda_{\bar{\rm{MS}}} = 318(12)(5) MeV and 292(5)(15) MeV respectively for these two methods, compatible which each other but significantly above the Schrodinger method estimate.Comment: 3 pages, LaTeX with two figures; presented at LATTICE9

    Paleoseismological analysis of late Miocene lacustrine successions in the Prebetic Zone, SE Spain

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    A paleoseismological study of late Miocene lacustrine sediments was carried out in the Neogene basins of the Prebetic Zone in Albacete (Spain). We developed a multidisciplinary methodology which could be used to extrapolate the paleoseismic data to the present day. This multidisciplinary approach includes different disciplines, i.e. stratigraphy, structural analysis, seismological analysis and paleoseismology. Paleoseismological analysis was focussed on both shallow and deep lake deposits given that these sediments behave differently in different deformation fields. The seismites formed in shallow sediments were generated by liquefaction and include: sand dikes, pillow structures and intruded and fractured gr avels. The deep lake deposits show varied structures, such as loop bedding, disturbed varved lamination, mixed layers and pseudonodules. Seismites indicate paleoearthquake magnitude intervals. The trends of the seismites are usually oriented ve ry close to the stress field trends (from the late Miocene to the Present): NW-SE and NE-SW trends. This constitutes a link between tectonics and seismites. The va rved annual sedimentation evidenced by the deep lake facies was used as a relative dating method. Mixed layers were employed as paleoseismic indicators to calculate the earthquake recurrence interval. The mean recurrence interval is close to 130 years (9446 years of total record with 73 dated events), one maximum interval of 454 years and one minimum interval of 23 years and the mean estimated magnitude value is 5.1. The Gutenberg-Richter relationship shows similar "b" values close to 0.86 from paleoseismological and seismological data. This suggests that the seismic conditions have been similar since the late Miocene

    The Pion Light-Cone Wave Function Phi_pi on the lattice: a partonic signal?

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    We determine the conditions required to study the pion light-cone wave function Phi_pi with a new method: a direct display of the partons constituting the pion. We present the preliminary results of a lattice computation of Phi_pi following this direction. An auxiliary scalar-quark is introduced. The spectroscopy of its bound states is studied. We observe some indications of a partonic behavior of the system of this scalar-quark and the anti-quark.Comment: 3 pages, 4 figures, Lattice2001(matrixelement

    Axonal T<sub>2</sub> estimation using the spherical variance of the strongly diffusion-weighted MRI signal.

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    In magnetic resonance imaging, the application of a strong diffusion weighting suppresses the signal contributions from the less diffusion-restricted constituents of the brain's white matter, thus enabling the estimation of the transverse relaxation time T &lt;sub&gt;2&lt;/sub&gt; that arises from the more diffusion-restricted constituents such as the axons. However, the presence of cell nuclei and vacuoles can confound the estimation of the axonal T &lt;sub&gt;2&lt;/sub&gt; , as diffusion within those structures is also restricted, causing the corresponding signal to survive the strong diffusion weighting. We devise an estimator of the axonal T &lt;sub&gt;2&lt;/sub&gt; based on the directional spherical variance of the strongly diffusion-weighted signal. The spherical variance T &lt;sub&gt;2&lt;/sub&gt; estimates are insensitive to the presence of isotropic contributions to the signal like those provided by cell nuclei and vacuoles. We show that with a strong diffusion weighting these estimates differ from those obtained using the directional spherical mean of the signal which contains both axonal and isotropically-restricted contributions. Our findings hint at the presence of an MRI-visible isotropically-restricted contribution to the signal in the white matter ex vivo fixed tissue (monkey) at 7T, and do not allow us to discard such a possibility also for in vivo human data collected with a clinical 3T system

    Fast k-NN classifier for documents based on a graph structure

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    In this paper, a fast k nearest neighbors (k-NN) classifier for documents is presented. Documents are usually represented in a high-dimensional feature space, where terms appeared on it are treated as features and the weight of each term reflects its importance in the document. There are many approaches to find the vicinity of an object, but their performance drastically decreases as the number of dimensions grows. This problem prevents its application for documents. The proposed method is based on a graph index structure with a fast search algorithm. It’s high selectivity permits to obtain a similar classification quality than exhaustive classifier, with a few number of computed distances. Our experimental results show that it is feasible the use of the proposed method in problems of very high dimensionality, such as Text Mining

    Power Corrections to Perturbative QCD and OPE in Gluon Green Functions

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    We show that QCD Green functions in Landau Gauge exhibit sizable O(1/Ό2)O(1/\mu^2) corrections to the expected perturbative behavior at energies as high as 10 GeV. We argue that these are due to a -condensate which does not vanish in Landau gauge.Comment: 3 pages 1 figure lattice2001 (gaugetheories

    Sedimentología de la Fm Escucha (Albiense inferior-medio) entre Estercuel y Crivillén (Teruel) en la Cubeta de Oliete (Cuenca Ibérica Central)

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    A stratigraphie and sedimentologic study about the Escucha Fm (Lower-Middle Albian) has been done in the Oliete Subbasin (Central Iberian Basin). This lithostratighapic unit was developped during the last moments of the second rift state (Upper Jurassic-Lower Cretaceous), that affected the Iberian Basin. Sixteen facies has been distinguished and gathered in five characteristic facies associations: flood plain, marshftaay margin, interdistributary bay, crevasse splay and distributary channel. These facies associations belong to different sedimentary subenvironments developped in the proximal sector of a deltaic depositional system. The vertical sedimentary evolution shows a trend to more continental conditions from base to top. Different Albian macroflora remains have been found in different stratigraphic levels
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