Informe de la Reunión Técnica Subregional sobre Realidad y Perspectivas del Cooperativismo en Argentina, Brasil, Chile, Paraguay y Uruguay

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Case study on the interchange of automotive parts between Chile, Argentina and Venezuela

Information Paper, No 16

Transporte del comercio exterior de Paraguay a través del corredor Argentina-Chile = Transport of Paraguay's exports through the Argentine-Chilean corridor

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Tectonics and kinematics of curved mountain belts: examples from the Andes and the Alps

Curved mountain belts have always fascinated geologists and geophysicists because of their peculiar structural setting and geodynamic mechanisms of formation. The need of studying orogenic bends arises from the numerous questions to which geologists and geophysicists have tried to answer to during the last two decades, such as: what are the mechanisms governing orogenic bends formation? Why do they form? Do they develop in particular geological conditions? And if so, what are the most favorable conditions? What are their relationships with the deformational history of the belt? Why is the shape of arcuate orogens in many parts of the Earth so different? What are the factors controlling the shape of orogenic bends? Paleomagnetism demonstrated to be one of the most effective techniques in order to document the deformation of a curved belt through the determination of vertical axis rotations. In fact, the pattern of rotations within a curved belt can reveal the occurrence of a bending, and its timing. Nevertheless, paleomagnetic data alone are not sufficient to constrain the tectonic evolution of a curved belt. Usually, structural analysis integrates paleomagnetic data, in defining the kinematics of a belt through kinematic indicators on brittle fault planes (i.e., slickensides, mineral fibers growth, SC-structures). My research program has been focused on the study of curved mountain belts through paleomagnetism, in order to define their kinematics, timing, and mechanisms of formation. Structural analysis, performed only in some regions, supported and integrated paleomagnetic data. In particular, three arcuate orogenic systems have been investigated: the Western Alpine Arc (NW Italy), the Bolivian Orocline (Central Andes, NW Argentina), and the Patagonian Orocline (Tierra del Fuego, southern Argentina). The bending of the Western Alpine Arc has been investigated so far using different approaches, though few based on reliable paleomagnetic data. Results from our paleomagnetic study carried out in the Tertiary Piedmont Basin, located on top of Alpine nappes, indicate that the Western Alpine Arc is a primary bend that has been subsequently tightened by further ~50° during Aquitanian-Serravallian times (23-12 Ma). This mid-Miocene oroclinal bending, superimposing onto a pre-existing Eocene nonrotational arc, is the result of a composite geodynamic mechanism, where slab rollback, mantle flows, and rotating thrust emplacement are intimately linked. Relying on our paleomagnetic and structural evidence, the Bolivian Orocline can be considered as a progressive bend, whose formation has been driven by the along-strike gradient of crustal shortening. The documented clockwise rotations up to 45° are compatible with a secondary-bending type mechanism occurring after Eocene-Oligocene times (30-40 Ma), and their nature is probably related to the widespread shearing taking place between zones of differential shortening. Since ~15 Ma ago, the activity of N-S left-lateral strike-slip faults in the Eastern Cordillera at the border with the Altiplano-Puna plateau induced up to ~40° counterclockwise rotations along the fault zone, locally annulling the regional clockwise rotation. We proposed that mid-Miocene strike-slip activity developed in response of a compressive stress (related to body forces) at the plateau margins, caused by the progressive lateral (southward) growth of the Altiplano-Puna plateau, laterally spreading from the overthickened crustal region of the salient apex. The growth of plateaux by lateral spreading seems to be a mechanism common to other major plateaux in the Earth (i.e., Tibetan plateau). Results from the Patagonian Orocline represent the first reliable constraint to the timing of bending in the southern tip of South America. They indicate that the Patagonian Orocline did not undergo any significant rotation since early Eocene times (~50 Ma), implying that it may be considered either a primary bend, or an orocline formed during the late Cretaceous-early Eocene deformation phase. This result has important implications on the opening of the Drake Passage at ~32 Ma, since it is definitely not related to the formation of the Patagonian orocline, but the sole consequence of the Scotia plate spreading. Finally, relying on the results and implications from the study of the Western Alpine Arc, the Bolivian Orocline, and the Patagonian Orocline, general conclusions on curved mountain belt formation have been inferred.

An Assessment of the Case for Monetary Union or Official Dollarization in Argentina, Brazil, Chile, Uruguay and Venezuela

We use a data set covering the whole period of Argentina's currency board and most of that spanned by the Mercosur trade agreement to examine the case for either a Latin American monetary union or monetary union with the USA (through official dollarization). Our econometric evidence using VAR techniques indicates that macroeconomic shocks are still so highly asymmetric in Latin America and between Latin American countries and the USA as to make monetary union or official dollarization somewhat doubtful policies.

Estudio comparativo del cariotipo en especies de Miltinea Ravenna, Phycella Lindl. y Rhodophiala C. Presl (Amaryllidaceae) de Chile

La familia Amaryllidaceae se encuentra distribuida en diversas regiones de Chile y Sudamérica. De los 11 géneros reconocidos por Ravenna, al menos tres de ellos presentan un reconocido potencial ornamental: Miltinea Ravenna, endémico de Chile y conformado por la especie Miltinea maulensis (Ravenna) Ravenna, Phycella Lindley, endémico de Chile, conformado por cuatro especies y distribuido desde el valle de Elqui hasta la altura de la región de Arauco y Rhodophiala C. Presl. presente en el sur de Brasil, Uruguay, Bolivia, Argentina y Chile conformado por un número aproximado de 40 especies. Actualmente, la información taxonómica tradicional para diferenciar los géneros presentes en Chile es insuficiente. Es por ello que se utilizó la citotaxonomía como una herramienta y fuente de evidencia taxonómica. El objetivo de esta investigación fue realizar un estudio comparativo de los cariotipos en representantes de tres géneros de Amaryllidaceae que crecen en Chile con el fin de ayudar a clarificar la posición taxonómica de ellos. Las especies analizadas fueron: Miltinea maulensis (Ravenna) Ravenna, Phycella australis Ravenna, Rhodophiala araucana (Phil.) Traub, Rhodophiala montana (Phil.) Traub, y Rhodophiala pratensis (Poepp.) Traub. Los resultados obtenidos indicaron que Miltinea maulensis y Phycella australis presentan características cariológicas muy similares, tanto en el número cromosómico, fórmula cariotípica e índices cromosómicos. Estas características permitirían considerar Miltinea como un sinónimo de Phycella. Por último, las tres especies de Rhodophiala analizadas comparten características citológicas muy similares, como por ejemplo, la presencia de una región NOR en el brazo largo del cromosoma 7, idéntico número cromosómico e índices de asimetría de los cariotipos casi iguales.

Klaus Müller–Bergh y Gilberto Mendonça Teles. Vanguardia Latinoamericana: Historia, crítica y documentos. Tomo V, Sudamérica. Chile y países del Plata: Argentina, Uruguay, Paraguay. Madrid: Vervuert – Iberoamericana, 2009, 420 p.

Fil: Videla de Rivero, Gloria.

Régimen político y gobiernos locales : los municipios en las constituciones de Argentina y Chile : un estudio comparativo

Se presentan los resultados de una investigación de carácter descriptivo, cuyo objetivo ha sido comparar las coincidencias y diferencias de las normas constitucionales de ambos países referidas a los gobiernos locales, para establecer correspondencias con los regimenes políticos (democracia-dictadura) que los originaron. Utilizamos en este caso el método del estudio comparativo entre naciones (cross-national), propuesto por Jördi Cais, según el cual «El análisis entre países es un tipo de análisis comparativo que posee un margen amplio de comparaciones posibles." Se utilizó además el método de análisis de contenido y la exégesis de los textos constitucionales para establecer los términos objeto de comparación. Las conclusiones señalan que las diferencias mas importantes se centran en la amplia potestad reglamentaria que eI texto de la constitución chilena otorga al poder central. Palabras clave: Constitución. Gobierno local. Régimen político. Forma de Estado. Autonomía. Descentralización. Participación.