El camp cañí. Folclore popular, kitsch y género en el arte contemporáneo español

Partiendo de la noción de camp, especialmente de la caracterización aportada por Susan Sontag, estudiaremos la estética kitsch y las influencias del folclore popular en el arte contemporáneo español, concretamente en el asociado al momento histórico de la Transición y al movimiento sociocultural de la Movida. Asimismo prestaremos particular atención a su uso en discursos queer y de disidencia de género. Para ello nos centraremos en la obra de autores como José Pérez Ocaña y Costus (pareja profesional formada por Enrique Naya y Juan Carrero), en cuyas producciones el kitsch, el tono paródico y el uso de elementos de la cultura popular (desde iconografía religiosa hasta imágenes inspiradas en la canción española) sirven de expresión a posturas que, al tiempo que transitan los márgenes del binarismo sexual, apuntan a una cierta politización en consonancia con las corrientes aperturistas del momento.

Puesta en valor de la arquitectura moderna residencial post-terremoto de 1944. San Juan – Argentina

La ciudad y su arquitectura testimonian las culturas que modelan y remodelan sus formas y espacios en el tiempo. Toda comunidad tiene derecho a un ambiente urbano apto para el desarrollo humano sustentable. Desarrollo sustentable, es aquel que asegura la satisfacción de las necesidades del presente, sin comprometer los recursos con que generaciones futuras puedan satisfacer las propias (Naciones Unidas, 1987). Significa el uso racional y responsable de toda clase de recursos, especialmente los no renovables, como el patrimonio arquitectónico. La ciudad de San Juan fue reconstruida bajo influencias de los postulados del Movimiento Moderno tras el terremoto de 1944 que destruyó casi la totalidad de sus edificios patrimoniales. La arquitectura moderna es considerada internacionalmente un patrimonio a legar a las generaciones futuras. En San Juan, las obras residenciales modernas corren el riesgo de ser transformadas o demolidas ante un posible reemplazo por nuevas obras más redituables, por la dinámica del desarrollo urbano y la ausencia de protección que preserve este patrimonio. Es objetivo de este trabajo promover el reconocimiento, valoración y protección, de obras patrimoniales residenciales, exponentes de la modernidad arquitectónica local.

Indian Ocean Region, ca. 1690 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Nova tabula Indiae Orientalis. It was published by Carolus Allard excudit, between 1690 and 1710. Scale [ca. 1:5,500,000]. Covers the Indian Ocean Region. Map in Latin. The image inside the map neatline is georeferenced to the surface of the earth and fit to the World Miller Cylindrical projected coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as drainage, roads, cities and other human settlements, territorial boundaries, shoreline features, and more. Relief shown pictorially.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

Southern, Central, & Eastern Africa, ca. 1730 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Carte de l'Afrique meridionale : ou pays entre la ligne & le cap de Bonne Esperance et l'isle de Madagascar, par la veuve de Nicolas Visscher avec privilege. It was published by Chez Henry de Leth, Marchand de l'Estampes près de la Boursse ca. 1730. Scale [ca. 1:12,250,000]. Covers portions of Southern, Central, and Eastern Africa. Map in French and Dutch.The image inside the map neatline is georeferenced to the surface of the earth and fit to the Africa Sinusoidal projected coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as drainage, cities and other human settlements, territorial boundaries, shoreline features, and more. Relief shown pictorially. Includes notes and insets: [Cabo de Bon Esperanca], Elevation du port et Mont Table au Cap de Bonne Esperance and Plan du port et Mont Table au Cap de Bonne Esperance.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

Lithologic, mineral, chemical and isotopic compositions of altered rocks with increasing distance across the eastern flank of the Juan de Fuca Ridge, ODP Leg 168 data

During ODP Leg 168, 10 sites were drilled across the eastern flank of the Juan de Fuca Ridge (JdFR), to examine the conditions of fluid-rock interaction in three distinct hydrothermal regimes (referred to as the Hydrothermal Transition (HT), Buried Basement (BB) and Rough Basement (RB) transects), extending over a ~120 km linear transect perpendicular to the spreading ridge. This was carried out in an attempt to constrain the conditions and processes that control the location, style and magnitude of low temperature (<150°C) fluid-rock interaction within this setting. This paper presents new data on the petrology, mineral chemistry and whole rock strontium and oxygen isotopic compositions of basalts from the eastern flank of the JdFR, in order to investigate the extent, style and sequence of low-temperature hydrothermal alteration and to establish how the hydrothermal regime evolved with time. Throughout the flank, a progressive sequence of low-temperature hydrothermal alteration has been identified, marked by changes in the dominant secondary mineral assemblage, changing from: chlorite+chlorite/smectite; to iron oyxhydroxide+celadonite; to saponite+/-pyrite; culminating at present with Ca- to CaMg(+/-Fe,Mn)-carbonate. The changes in secondary mineralogy have been used to infer a series of systematic shifts in the conditions of alteration that occurred as the basement moved off-axis and was progressively buried by sediment. In general, hydrothermal alteration of the uppermost oceanic crust commenced under open, oxidative conditions, with interaction between unmodified to slightly modified seawater and basaltic crust, to a regime in which circulation of a strongly modified seawater-derived fluid was more restricted, and alteration occurred under non-oxidative conditions. Across the flank, petrological observations and microprobe analyses indicate that the observed ranges in secondary mineral composition are directly related to changes in the geochemical and textural characteristics of the basement, as well as to interaction between fluids and phases from the four stages of alteration. This is suggestive of an increase in fluid-rock increased with time. Whole rock 87Sr/86Sr and d18O analyses of basalts from across the eastern flank of the JdFR reinforce petrological observations, with 87Sr/86Sr and d18O values slightly elevated above accepted pristine MORB values for this region. These results are consistent with an increase in the amount of fluid-rock interaction with time. Across the flank, enrichment in the 87Sr/86Sr and d18O relative to MORB, is influenced by a number of factors, including: local and regional variations in the crustal lithology and structure; the age of the crust; the extent of bulk rock alteration; and theoretically, the relative abundance of different isotopically-enriched secondary mineral phases in the crust.

Concentrations and isotopic compositions of low molecular weight hydrocarbons in hydrothermal fluids from ODP Field, Middle Valley, northern Juan de Fuca Ridge

The presence of sedimentary organic matter blanketing midocean ridge crests has a potentially strong impact on metal transport in hydrothermal vent fluids. To constrain the role of organic matter in metal mobility during hydrothermal sediment alteration, we reacted organic-rich diatomaceous ooze from Guaymas Basin, Gulf of California, and organic-poor hemipelagic mud from Middle Valley, northern Juan de Fuca Ridge, with seawater and a Na-Ca-K-Cl fluid of seawater chlorinity, at 275° to 400°C, 350 to 500 bars, and initial fluid: sediment mass ratios ranging from 1.6 to 9.8. Reaction of these fluids with both sediment types released CO2 and high concentrations of ore-forming metals (Fe, Mn, Zn, Pb) to solution. Relatively low concentrations of Cu were observed in solution and likely reflect the reducing conditions that resulted from the presence of sedimentary organic matter. Both the concentrations of CO2 and dissolved metals were lower in fluids reacted with Middle Valley sediment compared with aqueous concentrations in fluids reacted with Guaymas Basin sediment. During alteration of both sediment types, metal concentrations varied strongly as a function of temperature, increasing by up to an order of magnitude over the 75°C range of each experiment. Major element fluid chemistry and observed alteration assemblages suggest that during hydrothermal alteration of organic-lean sediment from Middle Valley a feldspar-quartz-illite mineral assemblage buffered in situ pH. In contrast, data from the experimental alteration of organic-rich Guaymas Basin sediment suggest that a calcite-plagioclase-quartz assemblage regulated in situ pH. Fluid speciation calculations suggest that in situ pH during Guaymas Basin sediment alteration was lower than during alteration of Middle Valley sediment and accounts for the substantially greater metal mobility at a given temperature and pressure during the former experiment. Comparison of our results with the results of basalt alteration experiments indicate that except for Cu, hydrothermal sediment alteration results in equal or greater concentrations of ore-forming metals at a given temperature and pressure. Accordingly, the presence of ore-forming metals in fluids currently venting from sediment-covered hydrothermal systems at concentrations substantially lower than in fluids from bare-rock systems may reflect chemical reequilibration during subsurface cooling within the sediment pile.

Crítica literaria.

Mode of access: Internet.

Memoria analictica de las aguas minerales sulfurosas frias de la fuente llamada de S. Juan en el pueblo de Guitiriz /

Antigua Signatura Ca 2799(20)

Historia crítica de España y de la cultura española /

Mode of access: Internet.

Historia crítica de la Inquisición en España : obra original conforme lo que resulta de los archivos del Consejo de la Suprema y de los tribunales de provincia /

La il. es un retr. del autor.

Comedias escogidas de don Juan Ruiz de Alarcón y Mendoza.

Contiene: Tomo 1,

Historia crítica de la Inquisición en España

Tomo X impreso en la Imprenta de Firmin Didot.

La vita di Maria uergine, di Caterina santa, & di Tomaso Aquinate, Beato /

Mode of access: Internet.

Cartas de Juan de la Encina /

Mode of access: Internet.

Historia crítica de España y de la cultura española en todo género /

Mode of access: Internet.