Chromite-silicate chemistry of the Neoarchean Sittampundi Complex, southern India: Implications for subduction-related arc magmatism

The Neoarchean layered anorthositic complex at Sittampundi in southern India is known for its chromitite layers that are mostly associated with anorthosite (An(90-100)). The chromitites contain FeAl-rich chromites concentrated in layers between amphibole-rich layers with a dominant mineralogy of amphibole-spinel-plagiocase+/-sapphirine. The chromite-rich layers contain only amphibole and plagioclase. Mineral compositions illustrated by X-ray composition maps and profiles show subtle chemical differences. The chrome spinels are of refractory grade with Cr2O3 and Al2O3 contents varying between 34-40 wt.% and 23-28 wt.%. The chromite compositions are noticeably different from those in layered igneous intrusions of the Bushveld-Stillwater type. The existence of original highly calcic plagioclase, FeAl-rich chromite, and magmatic amphibole is consistent with derivation from a parental magma of hydrous tholeiitic composition that was most likely generated in a supra-subduction zone arc setting. In terms of mineralogy and field relations, the Sittampundi chromitites are remarkably similar to anorthosite-hosted chromitites in the Neoarchean Fiskensset anorthositic complex, Greenland. We propose that the Sittampundi chromitites formed by partial melting of unusually aluminous harzburgite in a hydrated mantle wedge above a subduction zone. This melting process produced hydrous, aluminous basalt, which fractionated at depth to give rise to a variety of high-alumina basalt compositions from which the anorthositic complex with its cumulate chromite-rich and amphibole-rich layers formed within the magma chamber of a supra-subduction zone arc. (C) 2011 Elsevier B.V. All rights reserved.

Channel training signal design for reciprocal multiple antenna systems with beamforming

Fast and efficient channel estimation is key to achieving high data rate performance in mobile and vehicular communication systems, where the channel is fast time-varying. To this end, this work proposes and optimizes channel-dependent training schemes for reciprocal Multiple-Input Multiple-Output (MIMO) channels with beamforming (BF) at the transmitter and receiver. First, assuming that Channel State Information (CSI) is available at the receiver, a channel-dependent Reverse Channel Training (RCT) signal is proposed that enables efficient estimation of the BF vector at the transmitter with a minimum training duration of only one symbol. In contrast, conventional orthogonal training requires a minimum training duration equal to the number of receive antennas. A tight approximation to the capacity lower bound on the system is derived, which is used as a performance metric to optimize the parameters of the RCT. Next, assuming that CSI is available at the transmitter, a channel-dependent forward-link training signal is proposed and its power and duration are optimized with respect to an approximate capacity lower bound. Monte Carlo simulations illustrate the significant performance improvement offered by the proposed channel-dependent training schemes over the existing channel-agnostic orthogonal training schemes.

Power-Controlled Reverse Channel Training in a Multiuser TDD-MIMO Spatial Multiplexing System With CSIR

This paper considers the design of a power-controlled reverse channel training (RCT) scheme for spatial multiplexing (SM)-based data transmission along the dominant modes of the channel in a time-division duplex (TDD) multiple-input and multiple-output (MIMO) system, when channel knowledge is available at the receiver. A channel-dependent power-controlled RCT scheme is proposed, using which the transmitter estimates the beamforming (BF) vectors required for the forward-link SM data transmission. Tight approximate expressions for 1) the mean square error (MSE) in the estimate of the BF vectors, and 2) a capacity lower bound (CLB) for an SM system, are derived and used to optimize the parameters of the training sequence. Moreover, an extension of the channel-dependent training scheme and the data rate analysis to a multiuser scenario with M user terminals is presented. For the single-mode BF system, a closed-form expression for an upper bound on the average sum data rate is derived, which is shown to scale as ((L-c - L-B,L- tau)/L-c) log logM asymptotically in M, where L-c and L-B,L- tau are the channel coherence time and training duration, respectively. The significant performance gain offered by the proposed training sequence over the conventional constant-power orthogonal RCT sequence is demonstrated using Monte Carlo simulations.

Elastic thickness structure of the Andaman subduction zone: Implications for convergence of the Ninetyeast Ridge

We use the Bouguer coherence (Morlet isostatic response function) technique to compute the spatial variation of effective elastic thickness (T-e) of the Andaman subduction zone. The recovered T-e map resolves regional-scale features that correlate well with known surface structures of the subducting Indian plate and the overriding Burma plate. The major structure on the India plate, the Ninetyeast Ridge (NER), exhibits a weak mechanical strength, which is consistent with the expected signature of an oceanic ridge of hotspot origin. However, a markedly low strength (0< T-e <3 km) in that region, where the NER is close to the Andaman trench (north of 10 N), receives our main attention in this study. The subduction geometry derived from the Bouguer gravity forward modeling suggests that the NER has indented beneath the Andaman arc. We infer that the bending stresses of the viscous plate, which were reinforced within the subducting oceanic plate as a result of the partial subduction of the NER buoyant load, have reduced the lithospheric strength. The correlation, T-e < T-s (seismogenic thickness) reveals that the upper crust is actively deforming beneath the frontal arc Andaman region. The occurrence of normal-fault earthquakes in the frontal arc, low Te zone, is indicative of structural heterogeneities within the subducting plate. The fact that the NER along with its buoyant root is subducting under the Andaman region is inhibiting the subduction processes, as suggested by the changes in trench line, interrupted back-arc volcanism, variation in seismicity mechanism, slow subduction, etc. The low T-e and thinned crustal structure of the Andaman back-arc basin are attributed to a thermomechanically weakened lithosphere. The present study reveals that the ongoing back-arc spreading and strike-slip motion along the West Andaman Fault coupled with the ridge subduction exerts an important control on the frequency and magnitude of seismicity in the Andaman region. (C) 2013 Elsevier Ltd. All rights reserved.

A Rodinian suture in western India: New insights on India-Madagascar correlations

We report detailed evidence for a new paleo-suture zone (the Kumta suture) on the western margin of southern India. The c. 15-km-wide, westward dipping suture zone contains garnet-biotite, fuchsite-haematite, chlorite-quartz, quartz-phengite schists, biotite augen gneiss, marble and amphibolite. The isochemical phase diagram estimations and the high-Si phengite composition of quartz-phengite schist suggest a near-peak condition of c. 18 kbar at c. 550 degrees C, followed by near-isothermal decompression. The detrital SHRIMP U-Pb zircon ages from quartz-phengite schist give four age populations ranging from 3280 to 2993 Ma. Phengite from quartz-phengite schist and biotite from garnet-biotite schist have K-Ar metamorphic ages of ca. 1326 and ca. 1385 Ma respectively. Electron microprobe-CHIME ages of in situ zircons in quartz-phengite schist (ca. 3750 Ma and ca. 1697 Ma) are consistent with the above results. The Bondla ultramafic-gabbro complex in the west of the Kumta suture compositionally represents an arc with K-Ar biotite ages from gabbro in the range 1644-1536 Ma. On the eastern side of the suture are weakly deformed and unmetamorphosed shallow westward-dipping sedimentary rocks of the Sirsi shelf, which has the following upward stratigraphy: pebbly quartzite/sandstone, turbidite, magnetite iron formation, and limestone; farther east the lower lying quartzite has an unconformable contact with ca. 2571 Ma quartzo-feldspathic gneisses of the Dharwar block with a ca. 1733 Ma biotite cooling age. To the west of the suture is a c. 60-km-wide Karwar block mainly consisting of tonalite-trondhjemite-granodiorite (TTG) and amphibolite. The TTGs have U-Pb zircon magmatic ages of ca. 3200 Ma with a rare inherited core age of ca. 3601 Ma. The K-Ar biotite cooling age from the TTGs (1746 Ma and 1796 Ma) and amphibolite (ca. 1697 Ma) represents late-stage uplift. Integration of geological, structural and geochronological data from western India and eastern Madagascar suggest diachronous ocean closure during the amalgamation of Rodinia; in the north at around ca. 1380 Ma, and a progression toward the south until ca. 750 Ma. Satellite imagery based regional structural lineaments suggests that the Betsimisaraka suture continues into western India as the Kumta suture and possibly farther south toward a suture in the Coorg area, representing in total a c. 1000 km long Rodinian suture. (C) 2013 Elsevier B.V. All rights reserved.

Spatial variations of effective elastic thickness over the Ninetyeast Ridge and implications for its structure and tectonic evolution

We present new data on the strength of oceanic lithosphere along the Ninetyeast Ridge (NER) from two independent methods: spectral analysis (Bouguer coherence) using the fan wavelet transform technique, and spatial analysis (flexure inversion) with the convolution method. The two methods provide effective elastic thickness (T-e) patterns that broadly complement each other, and correlate well with known surface structures and regional-scale features. Furthermore, our study presents a new high resolution database on the Moho configuration, which obeys flexural isostasy, and exhibit regional correlations with the T-e variations. A continuous ridge structure with a much lower T-e value than that of normal oceanic lithosphere provides strong support for the hotspot theory. The derived T-e values vary over the northern (higher T-e similar to 10-20 km), central (anomalously low T-e similar to 0-5 km), and southern (low T-e similar to 5 km) segments of the NER. The lack of correlation of the T-e value with the progressive aging of the lithosphere implies differences in thermo-mechanical setting of the crust and underlying mantle in different parts of the NER, again indicating diversity in their evolution. The anomalously low T-e and deeper Moho (similar to 22 km) estimates of the central NER (between 0.5 degrees N and 17 degrees S) are attributed to the interaction of a hotspot with the Wharton spreading ridge that caused significant thermal rejuvenation and hence weakening of the lithosphere. The higher mechanical strength values in the northern NER (north of 0.5 degrees N) may support the idea of off-ridge emplacement and a relatively large plate motion at the time of volcanism. The low T-e and deeper Moho (similar to 22 km) estimates in the southern part (south of 17 degrees S) suggest that the lithosphere was weak and therefore younger at the time of volcanism, and this supports the idea that the southern NER was emplaced on the edge of the Indian plate. (C) 2013 Elsevier B.V. All rights reserved.

Tectonic inheritance of the Indian Shield: New insights from its elastic thickness structure

A new evaluation of the elastic thickness (Te) structure of the Indian Shield, derived from isotropic fan wavelet methodology, documents spatial variations of lithospheric deformation in different tectonic provinces correlated with episodic tectono-thermal events. The Te variations corroborated by shear velocity, crustal thickness, and seismogenic thickness reveal the heterogeneous rheology of the Indian lithosphere. The thinned, attenuated lithosphere beneath Peninsular India is considered to be the reason for its mechanically weak strength (<30 km), where a decoupled crust-mantle rheology under different surface/subsurface loading structures may explain the prominent low Te patterns. The arcuate Te structure of the Western Dharwar province and a NNE-trending band of low Te anomaly in the Southern Granulite Terrane are intriguing patterns. The average Te values (40-50 km) of the Central Indian Tectonic Zone, the Bastar Craton, and the northern Eastern Ghats Mobile Belt are suggestive of old, stable, Indian lithosphere, which was not affected by any major tectono-thermal events after cratonic stabilization. We propose that the anomalously high Te (60-85 km) and high S-wave velocity zone to the north of the Narmada-Son Lineament, mainly in NW Himalaya, and the northern Aravalli and Bundelkhand Cratons, suggest that Archean lithosphere characterized by a high velocity mantle keel supports the orogenic topographic loads in/near the Himalaya. The Te map clearly segments the volcanic provinces of the Indian Shield, where the signatures of the Reunion, Marion, and Kerguelen hotspots are indicated by significantly low Te patterns that correlate with plume- and rift-related thermal and mechanical rejuvenation, magmatic underplating, and crustal necking. The correlations between Te variations and the occurrence of seismicity over seismically active zones reveal different causal relationships, which led to the current seismogenic zonation of the Indian Shield. (C) 2013 Elsevier B.V. All rights reserved.

India-Madagascar paleo-fit based on flexural isostasy of their rifted margins

The present study contributes new constraints on, and definitions of, the reconstructed plate margins of India and Madagascar based on flexural isostasy along the Western Continental Margin of India (WCMI) and the Eastern Continental Margin of Madagascar (ECMM). We have estimated the nature of isostasy and crustal geometry along the two margins, and have examined their possible conjugate structure. Here we utilize elastic thickness (Te) and Moho depth data as the primary basis for the correlation of these passive margins. We employ the flexure inversion technique that operates in spatial domain in order to estimate the spatial variation of effective elastic thickness. Gravity inversion and flexure inversion techniques are used to estimate the configuration of the Moho/Crust-Mantle Interface that reveals regional correlations with the elastic thickness variations. These results correlate well with the continental and oceanic segments of the Indian and African plates. The present study has found a linear zone of anomalously low-Te (1-5 km) along the WCMI (similar to 1680 km), which correlates well with the low-Te patterns obtained all along the ECMM. We suggest that the low-Te zones along the WCMI and ECMM represent paleo-rift inception points of lithosphere thermally and mechanically weakened by the combined effects of the Marion hotspot and lithospheric extension due to rifting. We have produced an India-Madagascar paleo-fit representing the initial phase of separation based on the Te estimates of the rifted conjugate margins, which is confirmed by a close-fit correlation of Moho geometry and bathymetry of the shelf margins. The matching of tectonic lineaments, lithologies and geochronological belts between India and Madagascar provide an additional support for the present plate reconstruction. (C) 2014 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.

Structure-mechanical property correlations in mechanochromic luminescent crystals of boron difluoride dibenzoylmethane derivatives

The structure and mechanical properties of crystalline materials of three boron difluoride dibenzoylmethane (BF(2)dbm) derivatives were investigated to examine the correlation, if any, among mechanochromic luminescence (ML) behaviour, solid-state structure, and the mechanical behaviour of single crystals. Qualitative mechanical deformation tests show that the crystals of BF(2)dbm(Bu-t)(2) can be bent permanently, whereas those of BF(2)dbm(OMe)(2) exhibit an inhomogeneous shearing mode of deformation, and finally BF(2)dbmOMe crystals are brittle. Quantitative mechanical analysis by nanoindentation on the major facets of the crystals shows that BF(2)dbm(Bu-t)(2) is soft and compliant with low values of elastic modulus, E, and hardness, H, confirming its superior suceptibility for plastic deformation, which is attributed to the presence of a multitude of slip systems in the crystal structure. In contrast, both BF(2)dbm(OMe)(2) and BF(2)dbmOMe are considerably stiffer and harder with comparable E and H, which are rationalized through analysis of the structural attributes such as the intermolecular interactions, slip systems and their relative orientation with respect to the indentation direction. As expected from the qualitative mechanical behaviour, prominent ML was observed in BF(2)dbm(Bu-t)(2), whereas BF(2)dbm(OMe)(2) exhibits only a moderate ML and BF(2)dbmOMe shows no detectable ML, all examined under identical conditions. These results confirm that the extent of ML in crystalline organic solid-state fluorophore materials can be correlated positively with the extent of plasticity (low recovery). In turn, they offer opportunities to design new and improved efficient ML materials using crystal engineering principles.

Linking monazite geochronology with fluid infiltration and metamorphic histories: Nature and experiment

Migmatised metapelites from the Kodaikanal region, central Madurai Block, southern India have undergone ultrahigh-temperature metamorphism (950-1000 degrees C; 7-8 kbar). In-situ electron microprobe Th-U-Pb isochron (CHIME) dating of monazites in a leucosome and surrounding silica-saturated and silica-poor restites from the same outcrop indicates three principal ages that can be linked to the evolutionary history of these rocks. Monazite grains from the silica-saturated restite have well-defined, inherited cores with thick rims that yield an age of ca. 1684 Ma. This either dates the metamorphism of the original metapelite or is a detrital age of inherited monazite. Monazite grains from the silica-poor restite, thick rims from the silica-saturated restite, and monazite cores from the leucosome have ages ranging from 520 to 540 Ma suggesting a mean age of 530 Ma within the error bars. In the leucosome the altered rim of the monazite gives an age of ca. 502 Ma. Alteration takes the form of Th-depleted lobes of monazite with sharp curvilinear boundaries extending from the monazite grain rim into the core. We have replicated experimentally these altered rims in a monazite-leucosome experiment at 800 degrees C and 2 kbar. This experiment, coupled with earlier published monazite-fluid experiments involving high pH alkali-bearing fluids at high P-T, helps to confirm the idea that alkali-bearing fluids, in the melt and along grain boundaries during crystallization, were responsible for the formation of the altered monazite grain rims via the process of coupled dissolution-reprecipitation. (C) 2015 Elsevier B.V. All rights reserved.

Evolution of high-pressure mafic granulites and pelitic gneisses from NE Madagascar: Tectonic implications

The occurrence of high-pressure mafic-ultramafic bodies within major shear zones is one of the indicators of paleo-subduction. In mafic granulites of the Andriamena complex (north-eastern Madagascar) we document unusual textures including garnet-clinopyroxene-quartz coronas that formed after the breakdown of orthopyroxene-plagioclase-ilmenite. Textural evidence and isochemical phase diagram calculations in the Na2O-CaO-K2O-FeO-MgO-Al2O3-SiO2-H2O-TiO2 system indicate a pressure-temperature (P-T) evolution from an isothermal (780 degrees C) pressure up to c. 24 kbar to decompression and cooling. Such a P-T trajectory is typically attained in a subduction zone setting where a gabbroic/ultramafic complex is subducted and later exhumed to the present crustal level during oceanic closure and final continental collision. The present results suggest that the presence of such deeply subducted rocks of the Andriamena complex is related to formation of the Betsimisaraka suture. LA-ICPMS U-Pb zircon dating of pelitic gneisses from the Betsimisaraka suture yields low Th/U ratios and protolith ages ranging from 2535 to 2625 Ma. A granitic gneiss from the Alaotra complex yields a zircon crystallization age of ca. 818 Ma and Th/U ratios vary from 1.08 to 2.09. K-Ar dating of muscovite and biotite from biotite-kyanite-sillimanite gneiss and garnet-biotite gneiss yields age of 486 +/- 9 Ma and 459 +/- 9 Ma respectively. We have estimated regional crustal thicknesses in NE Madagascar using a flexural inversion technique, which indicates the presence of an anomalously thick crust (c. 43 km) beneath the Antananarivo block. This result is consistent with the present concept that subduction beneath the Antananarivo block resulted in a more competent and thicker crust. The textural data, thermodynamic model, and geophysical evidence together provide a new insight to the subduction history, crustal thickening and evolution of the high-pressure Andriamena complex and its link to the terminal formation of the Betsimisaraka suture in north-eastern Madagascar. (C) 2015 Elsevier B.V. All rights reserved.

Autoconcepto y calidad de vida en niños entre 8 y 12 años que concurren a los hogares de tránsito de la ciudad de Concepción del Uruguay, Entre Ríos

Resumen: La presente investigación, de tipo descriptiva-correlacional y transversal, se centró en conocer la relación que existe entre el autoconcepto y la calidad de vida de los niños entre 8 y 12 años que concurren a los hogares de tránsito, en la ciudad de Concepción del Uruguay, Entre Ríos. La muestra (no probabilística, intencional) estuvo conformada por 64 niños, de ambos sexos, 33 varones y 31 mujeres. Los mismos tenían entre 8 y 12 años. Los individuos evaluados eran asistentes a los hogares de tránsito mencionados anteriormente. Las técnicas de recolección de datos utilizadas fueron las siguientes: la Escala Verbal para Niños y Adolescentes del Autoconcepto de Martina Casullo, adaptación de Piers-Harris (1964) y el Cuestionario para Calidad de Vida Kidscreen-27. La Escala Verbal para Niños y Adolescentes del Autoconcepto (Casullo, 1990), cuenta con seis dimensiones: comportamiento, estatus intelectual y escolar, imagen corporal, sentimientos de ansiedad, percepciones acerca del reconocimiento que otros hacen de la propia conducta (popularidad) y bienestar y satisfacción personal. El cuestionario Kidscreen-27 (Quintero, Lugo, García, y Sánchez, 2011) consta de cinco dimensiones: actividad física y salud, estado de ánimo y sentimientos, vida familiar y tiempo libre, apoyo social y amigos, y entorno escolar. Los datos fueron recabados por medio de la concurrencia a ambos hogares, solicitando previamente las autorizaciones correspondientes a los directivos, como así también a los padres y/o tutores de los niños. Respecto a los procedimientos de análisis de los datos, se utilizó el programa estadístico informático SPSS (Statistical Package for the Social Sciences) versión 15.0 para Windows. Se realizó un análisis descriptivo de las dos variables principales de esta investigación (autoconcepto y calidad de vida) con el objetivo de conocer los niveles con que se presentan en niños. Además, para conocer la relación entre ambas variables, se llevó a cabo el análisis de correlación de Pearson. Para estudiar si existe diferencia en el autoconcepto y la calidad de vida en función del sexo de los niños, se realizó análisis multivariados de varianza (MANOVA). Los resultados obtenidos indicaron niveles elevados en la mayoría de las dimensiones de las variables estudiadas (autoconcepto y calidad de vida). En cuanto a las distinciones según el sexo en dichas variables, no se encontraron diferencias significativas, sólo una variación mínima en dos dimensiones del autoconcepto, donde se visualiza que el comportamiento social y la popularidad es más elevada en los niños que en las niñas.Se hallaron, por otro lado, correlaciones estadísticamente significativas en la mayoría de las dimensiones de ambas variables, las mismas son: entre comportamiento y actividad física/salud; entre comportamiento y apoyo social/amigos; entre comportamiento y entorno escolar; entre estatus intelectual/escolar y actividad física/salud; entre estatus intelectual/escolar y estado de ánimo/sentimientos; entre estatus intelectual/escolar y entorno escolar; entre imagen corporal con apoyo social/amigos; entre sentimientos de ansiedad y actividad física/salud; entre sentimientos de ansiedad y estado de ánimo/sentimientos; entre sentimientos de ansiedad y apoyo social/amigos; entre popularidad y estado de ánimo/sentimientos; entre popularidad y apoyo social/amigos; entre bienestar/satisfacción vital y actividad física/salud; entre bienestar/satisfacción vital y estado de ánimo/sentimientos; entre bienestar/satisfacción vital y apoyo social/amigos; entre bienestar/satisfacción vital y entorno escolar; entre el total global del autoconcepto y actividad física/salud; entre el total global del autoconcepto y estado de ánimo/sentimientos; entre el total global del autoconcepto y apoyo social/amigos; entre el total global del autoconcepto y entorno escolar. Sólo una dimensión de la calidad de vida no se relaciona con ninguna de las dimensiones del autoconcepto, a saber, vida familiar/tiempo libre. En lo que respecta a las conclusiones, puede considerarse que los resultados de esta investigación verifican que existe correlación entre el autoconcepto y la calidad de vida de los niños concurrentes a los hogares de tránsito Santa Clara de Asís y la Casa del Menor

Calidad de vida en adultos con diagnóstico de psoriasis de la ciudad de Paraná : diferencias según sexo

Resumen: La presente investigación tuvo como objetivo evaluar la percepción de la calidad de vida en aquellos adultos con diagnóstico de psoriasis de la ciudad de Paraná y conocer diferencias según sexo. El diseño de investigación fue de tipo descriptivo – correlacional, transversal y de campo; el muestreo fue intencional no probabilístico. Con una muestra compuesta por 36 sujetos de ambos sexo, de 18 a 65 años. Los instrumentos que se aplicaron fueron el World Health Organization Quality of Life Questionaire (WHOQOL-100), en su versión Argentina (Bonicatto y Soria, 1998), junto con dos cuestionarios ad hoc, uno sociodemográfico y otro para explorar la imagen corporal. El procesamiento de la información obtenida a través del WHOQOL-100 se realizó mediante el programa Stadistical Package for the Social Sciences (SPSS) 21. Mientras que los ítems del cuestionario ad hoc de imagen corporal fueron evaluados cualitativamente de manera individual, las respuestas fueron agrupadas por categorías y luego se obtuvieron las frecuencias, porcentajes y análisis de contenido. Se observó que los adultos con diagnóstico de psoriasis de la ciudad de Paraná presentaron en general, una buena calidad de vida. Se determinó que existen diferencias según sexo, las mujeres obtuvieron mayores puntajes en los dominios Relaciones Sociales y Espiritualidad, como también en las facetas de sentimientos positivos, relaciones personales, seguridad física y espiritualidad. Por último, se observó que la imagen corporal se vio afectada por dicha enfermedad en la muestra estudiada

El tertium narrativo de los Evangelios : paradigma de un lenguaje nuevo desde la óptica ricoeuriana de Adolphe Gesché

Introducción: En las obras de Adolphe Gesché (1928-2003) aparecen temáticas que echan sus raíces en la teología dogmática y en la fundamental. Realiza su camino académico de licenciatura en filosofía y letras en la Universidad Católica de Lovaina, donde también, posteriormente, se licencia y doctora en teología. Más tarde realiza su magíster con una tesis sobre patrología. Si bien nunca faltarán en su madurez bibliográfica estos recursos de la primera hora, enfocará sus investigaciones y desarrollos hacia horizontes más dogmáticos. Estos últimos serán tratados desde abordajes múltiples, como la moral, la antropología, la psicología, filosofía y estética, la literatura y la teología comparada. Es precisamente en esta nota o personalidad de su “teologizar desde el encuentro” donde radicará la disertación presente, subrayando la riqueza de variados afluentes y detectando esas pistas de enlaces o convergencias que abren la posibilidad de la aplicación interdisciplinaria y del diálogo entre esos campos. Cabe destacar en Gesché el sustrato de diálogo con otras áreas humanísticas debido a sus estudios en humanidades y en filosofía y letras realizados en la Facultad de Saint Louis, Bruselas, previos a su ordenación sacerdotal. Gesché se esfuerza en sus obras por proveerse de un método interno y, al mismo tiempo, de una propuesta metodológica para futuras investigaciones. Lo confirmará el teólogo mismo al decir que “este recorrido constituye una experiencia que deseo realizar, tanto más que, a mi juicio, resulta decisiva para nuestra postmodernidad”. Se utilizará como material fuente su obra teológica magna sistematizada en siete tomos que llevan por título “Dios para pensar”, pero esto no impedirá recurrir a textos de algunas otras obras de su autoría y a su Fichero temático personal. La disertación apuntará al estudio de la importancia que Gesché confiere a la dimensión narrada del evangelio como principal fuente de luz sobre la persona e identidad de Jesucristo, constituyéndose en un modelo de relato que configura la identidad de aquel que narra, ejerciendo, también, una eficacia para aquel que lo lee. Texto, sujeto y lector serán, entonces, los ejes de su estudio y, también, la estructura de la disertación. Es el evangelio, en su esencia “narrado”, el que confiere identidad a la persona de Jesucristo. Esta dimensión narrativa del texto evangélico supera dos polos generados en la tradición teológica apoyados uno en la historia y el otro en el dogma. Ésta será la principal tesis sostenida por el teólogo y planteará el advenimiento de un tercero para resolver el ahogo de los encierros narcisistas...

El tinkunaco riojano : experiencia de religiosidad popular interpretada desde las categorías de fiesta y diálogo

Introducción: El Tinkunaco en la provincia de La Rioja, Argentina, es una fiesta que, arraigada en este pueblo desde 1593, tiene una hondura inigualable. Puede ser leída desde diversos ángulos: realizando un recorrido histórico a lo largo de sus más de 400 años de historia, estudiándola desde la teología, la etnografía, el folklore, la lingüística, la política. Cada ciencia y línea de investigación tendrá su propio método, pero separadas unas de otras no accederán acabadamente a la fiesta. Nosotros realizaremos en esta tesis un acercamiento desde la Teología Práctica integrando también a ciencias tales como la historia, la sociología, la psicología...