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Máscaras de la diablada puneñaBegazo Medina, Luciana 02 December 2021 (has links)
En el presente trabajo de investigación, se desarrolla el origen, significado y evolución de las máscaras de la diablada puneña, mediante la recopilación de diversas fuentes de información, en donde se rescata el testimonio de artesanos, bailarines y pobladores puneños. La investigación plantea el siguiente objetivo: Diseñar una colección de moda street wear femenina a partir del análisis teórico y visual de las máscaras de la diablada puneña.
Respecto al desarrollo de antecedentes, solo se encontraron antecedentes nacionales. Esto se debe porque las máscaras de la diablada puneña, es un tema netamente local. De esta manera, el presente trabajado de investigación se desarrolla en base a artistas peruanos. En el estado del arte, se ha entrevistado a expertos en el tema de investigación propuesto, como mascareros y diseñadores para consolidar la información recogida, la cual ha aportado al desarrollo de definiciones y datos relevantes en el presente trabajo de investigación.
Asimismo, en base a la teorización de las máscaras de la diablada puneña, se ha desarrollado un proceso visual con moodboards, prototipos de estructuras y volúmenes. En complemento, se realizo un perfil del usuario, lo que permitió realizar bocetos con la descripción analizada. El resultado final, evidencia una relación entre los elementos de las máscaras de la diablada puneña en el proceso creativo, plasmado en cada indumento propuesto. / In this research work, the origin, meaning and evolution of the masks of the diablada puneña are developed, through the compilation of various sources of information, where the testimony of artisans, dancers and residents of Puno is rescued. The research raises the following general objective: Design a collection of women's street wear fashion based on the theoretical and visual analysis of the masks of the devil from Puno.
Regarding the development of antecedents, only national antecedents were found. This is because the masks of the diablada puneña, is a purely local theme. In this way, the present research work is developed based on Peruvian artists. In the state of the art, experts in the proposed research topic, such as mask makers and designers, have been interviewed to consolidate the information collected, which has contributed to the development of definitions and relevant data in this research work.
Likewise, based on the theorization of the masks of the diablada puneña, a visual process has been developed with moodboards, prototypes of structures and volumes. In addition, a user profile was made, which allowed making sketches with the analyzed description. The final result shows a relationship between the elements of the masks of the diablada puneña in the creative process, embodied in each proposed outfit. / Trabajo de investigación
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Geology and Origin of the Breccias in the Morenci-Metcalf District, Greenlee County, ArizonaBennett, Kenneth Carlton January 1975 (has links)
Rocks of the Morenci-Metcalf district consist of Precambrian metaquartzite-schist, granodiorite, and granite overlain by Paleozoic and Mesozoic sediments. Intrusion of igneous rocks, emplacement of breccia masses, and associated hydrothermal activity occurred in Laramide time. Breccias of the district are associated with the youngest sialic intrusive complex. This sequence includes intrusion of the Older Granite Porphyry stock, main stage district hydrothermal alteration, quartz veining, breccia formation, main stage district hydrothermal mineralization, and intrusion of the Younger Granite Porphyry plug. Breccia formation in the Morenci-Metcalf district is similar to breccia descriptions reported in the literature for other porphyry copper deposits. Three breccia types, of separate and distinct origins, are herein described as the Morenci, Metcalf and King, and Candelaria Breccias. The Morenci Breccia is an intrusion breccia that has formed along a pre-existing structural feature during the ascent and emplacement of the Older Granite Porphyry stock. It exhibits an oblate lenticular shape with angular to subrounded fragments in a matrix of quartz, K-feldspar, biotite, and minor rock flour. The Metcalf-King Breccias and numerous smaller breccia masses are the remnants of an original Older Granite Porphyry mantle above the ascending Younger Granite Porphyry complex. The breccia masses occur as large 'xenoliths' floating within the Younger Granite Porphyry plug and were formed by surging and collapse during emplacement of this intrusive. Fragments in the Metcalf and King Breccias grade from angular in the central core to rounded at the contacts and occur in a matrix of sericite, K- feldspar, quartz, and rock flour. The Candelaria Breccia is an explosion pipe and is the largest continuous breccia mass in the district. It is oval with an inverted cone appearance consisting of angular to subangular equidimensional fragments in a matrix of sericite, quartz, specularite, and rock flour. All the breccia masses occur within and subsequent to the district phyllic (quartz-sericite-pyrite) alteration zone. Main stage district copper mineralization postdates emplacement of the Older Granite Porphyry stock and breccia formation, and is prior to the intrusion of the Younger Granite Porphyry plug. Late stage quartz-sericite-pyrite-chalcopyrite veinlets occur in the Metcalf-King Breccia group. Field mapping and laboratory studies indicate that the Older Granite Porphyry stock appears to have been the main district mineralizer.
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