El desarrollo de las propiedades textuales, como herramienta para la enseñanza de la producción de textos no literarios, en el décimo año de educación básica de los colegios fiscales de la parroquia Ignacio Flores de la ciudad de Latacunga, provincia de Cotopaxi

Para la enseñanza de la escritura, en nuestro país, durante muchos años, los maestros y maestras se han basado en la gramática estructural, sin ningún buen resultado, ya que esta da prioridad únicamente al aspecto formal de la escritura y es el caso particular de los colegios Luis Fernando Ruiz y Trajano Naranjo Iturralde. Por esta razón, el primer capítulo de esta propuesta se centra en un nuevo enfoque, el de la Gramática Textual, dando a conocer los planteamientos de cada uno de los lingüistas y pedagogos como: Noam Chomsky, Teun A.van Dijk, Daniel Cassany, entre otros, sobre los procesos de la producción de textos. Además se hace una reflexión sobre lo que es escribir, los procesos cognitivos de la escritura y la importancia de enseñar a partir de situaciones comunicativas en que se use la escritura. En el segundo capítulo se realiza un análisis de la información recogida respecto al proceso que siguen los docentes de Lengua y Literatura para la enseñanza de la producción textual. También se analiza las encuestas realizadas a los estudiantes sobre cómo aprenden a escribir y las producciones textuales de los mismos, aplicando cada una de las propiedades textuales. En el tercer capítulo se describe la nueva propuesta de la Gramática Textual en la producción de textos no literarios, siguiendo cada uno de los pasos para escribir, sugeridos por los expertos. Además se realiza un ejemplo de planificación para la construcción de una noticia con los estudiantes del décimo año de educación básica, en la que se hace hincapié en la responsabilidad que tiene el maestro como mediador para brindar el grado de ayuda que requiere el estudiante en la aplicación de las propiedades textuales, hasta que consiga ser autónomo.

The Rondonian-San Ignacio Province in the SW Amazonian Craton: An overview

The Rondonian-San Ignacio Province (1.56-1.30 Ga) is a composite orogen created through successive accretion of arcs, ocean basin closure and final oblique microcontinent-continent collision. The effects of the collision are well preserved mostly in the Paragua Terrane (Bolivia and Mato Grosso regions) and in the Alto Guapore Belt and the Rio Negro-Juruena Province (Rondonia region), considering that the province was affected by later collision-related deformation and metamorphism during the Sunsas Orogeny (1.25-1.00 Ga). The Rondonian-San Ignacio Province comprises: (1) the Jauru Terrane (1.78-1.42 Ga) that hosts Paleoproterozoic basement (1.78-1.72 Ga), and the Cachoeirinha (1.56-1.52 Ga) and the Santa Helena (1.48-1.42 Ga) accretionary orogens, both developed in an Andean-type magmatic arc; (2) the Paragua Terrane (1.74-1.32 Ga) that hosts pre-San Ignacio units (>1640 Ma: Chiquitania Gneiss Complex, San Ignacio Schist Group and Lomas Manechis Granulitic Complex) and the Pensamiento Granitoid Complex (1.37-1.34 Ga) developed in an Andean-type magmatic arc; (3) the Rio Alegre Terrane (1.51-1.38 Ga) that includes units generated in a mid-ocean ridge and an intra-oceanic magmatic arc environments; and (4) the Alto Guapore Belt (<1.42-1.34 Ga) that hosts units developed in passive marginal basin and intra-oceanic arc settings. The collisional stage (1.34-1.32 Ga) is characterized by deformation, high-grade metamorphism, and partial melting during the metamorphic peak, which affected primarily the Chiquitania Gneiss Complex and Lomas Manechis Granulitic Complex in the Paragua Terrane, and the Colorado Complex and the Nova Mamore Metamorphic Suite in the Alto Guapore Belt. The Paragua Block is here considered as a crustal fragment probably displaced from its Rio Negro-Juruena crustal counterpart between 1.50 and 1.40 Ga. This period is characterized by extensive A-type and intra-plate granite magmatism represented by the Rio Crespo Intrusive Suite (ca. 1.50 Ga), Santo Antonio Intrusive Suite (1.40-1.36 Ga), and the Teotonio Intrusive Suite (1.38 Ga). Magmatism of these types also occur at the end of the Rondonian-San Ignacio Orogeny, and are represented by the Alto Candeias Intrusive Suite (1.34-1.36 Ga), and the Sao Lourenco-Caripunas Intrusive Suite (1.31-1.30 Ga). The cratonization of the province occurred between 1.30 and 1.25 Ga. (C) 2009 Elsevier Ltd. All rights reserved.

The Rondonian-San Ignacio Province in the SW Amazonian Craton: An overview

The Rondonian-San Ignacio Province (1.56-1.30 Ga) is a composite orogen created through successive accretion of arcs, ocean basin closure and final oblique microcontinent-continent collision. The effects of the collision are well preserved mostly in the Paragua Terrane (Bolivia and Mato Grosso regions) and in the Alto Guapore Belt and the Rio Negro-Juruena Province (Rondonia region), considering that the province was affected by later collision-related deformation and metamorphism during the Sunsas Orogeny (1.25-1.00 Ga). The Rondonian-San Ignacio Province comprises: (1) the Jauru Terrane (1.78-1.42 Ga) that hosts Paleoproterozoic basement (1.78-1.72 Ga), and the Cachoeirinha (1.56-1.52 Ga) and the Santa Helena (1.48-1.42 Ga) accretionary orogens, both developed in an Andean-type magmatic arc; (2) the Paragua Terrane (1.74-1.32 Ga) that hosts pre-San Ignacio units (>1640 Ma: Chiquitania Gneiss Complex, San Ignacio Schist Group and Lomas Manechis Granulitic Complex) and the Pensamiento Granitoid Complex (1.37-1.34 Ga) developed in an Andean-type magmatic arc; (3) the Rio Alegre Terrane (1.51-1.38 Ga) that includes units generated in a mid-ocean ridge and an intra-oceanic magmatic arc environments; and (4) the Alto Guapore Belt (<1.42-1.34 Ga) that hosts units developed in passive marginal basin and intra-oceanic arc settings. The collisional stage (1.34-1.32 Ga) is characterized by deformation, high-grade metamorphism, and partial melting during the metamorphic peak, which affected primarily the Chiquitania Gneiss Complex and Lomas Manechis Granulitic Complex in the Paragua Terrane, and the Colorado Complex and the Nova Mamore Metamorphic Suite in the Alto Guapore Belt. The Paragua Block is here considered as a crustal fragment probably displaced from its Rio Negro-Juruena crustal counterpart between 1.50 and 1.40 Ga. This period is characterized by extensive A-type and intra-plate granite magmatism represented by the Rio Crespo Intrusive Suite (ca. 1.50 Ga), Santo Antonio Intrusive Suite (1.40-1.36 Ga), and the Teotonio Intrusive Suite (1.38 Ga). Magmatism of these types also occur at the end of the Rondonian-San Ignacio Orogeny, and are represented by the Alto Candeias Intrusive Suite (1.34-1.36 Ga), and the Sao Lourenco-Caripunas Intrusive Suite (1.31-1.30 Ga). The cratonization of the province occurred between 1.30 and 1.25 Ga. (C) 2009 Elsevier Ltd. All rights reserved.

Ignacio de Assis Silva e os estudos literários

This paper aims to honor the semiotician Ignacio Assis Silva printed by the intensity in all his activities, emphasizing mainly on the accuracy insightful essays, which made him not only one of the most important promoters of semiotics greimasian in Brazil, but one of those responsible for its development. It should be noted also that he served with dedication in the Postgraduate Program in Literary Studies FCL/Araraquara UNESP, including efforts since its founding. The program owes much to him and others of FCL semioticians for the healthy integration between programs, Linguistics/Portuguese Language and Literary Studies. The latter was even initially, a literature program focusing on semiotics greimasian. Join together with all his persistent interest in building a "theory of language", which deeply and tenaciously pursued in their classes and in their texts and can be detected in Figurativização e metamorfose: o mito de Narciso (1995).

Metamorfose: reflexões sobre o pensamento de Ignacio Assis Silva ou tentando achar o fio da meada

This text, homage to Ignacio Assis Silva, looks for the founding theoretical conceptions of his thoughts. When I looked at his texts, from the 70’s to the 90’s, my reading went through the path of an author who is always worried about revealing the birthplace of meaning. To catch this unique moment of semiosis, Silva proposes the concept of metamorphosis, a key-term which allows us to unite the two ends of his formation: Historical Grammar and Semiotic

El género memorias en las últimas novelas de Ignacio Solares

Fil: Gambetta Chuk, Aída Nadí.

Voces desde la historia : Ignacio Solares y la novela de la revolución mexicana

A partir de los nuevos paradigmas que conocemos como Novelas Históricas Posmodernas, el escritor mexicano retoma esa extensa línea temática que se origina en el acontecimiento histórico que convulsionó, a principios del siglo XX, la extensa geografía mexicana. El objetivo de este trabajo es abarcar el estudio de las tres novelas de Solares que se ocupan de textualizar episodios de la Revolución: Madero, el otro, de 1989, La noche de Ángeles, de 1991, Columbus, 1996. La elección de las figuras manifiesta la intención de devolverles su verdadera voz desde esa mirada que sólo permite la ficción, en tanto los hechos contados surgieron “más de lo simbólicamente verdadero que de lo históricamente exacto". La atención estará en destacar la presencia de voces que, desde una particular focalización, se ocuparán de insertar en el discurso modalizaciones diversas. Estas voces habrán de problematizar, con mayor o menor intensidad según los diversos registros, impugnando, cuestionando o rescatando ciertos actos oscuros del pasado, llevados a cabo por quienes protagonizaron la gesta revolucionaria. El tono apelativo característico explicita, por otra parte, el lugar desde el cual la historia debe ser leída.