Evaluating stress patterns for Plio-Quaternary brittle deformation along the Calama-Olacapato-El Toro fault zone, Central Andes

Understanding the geometry and kinematics of the major structures of an orogen is important to elucidate its style of deformation, as well as its tectonic evolution. We describe the temporal and spatial changes in the state of stress of the trans-orogen area of the Calama-Olacapato-El Toro (COT) Fault Zone in the Central Andes, at about 24°S within the northern portion of the Puna Plateau between the Argentina-Chile border. The importance of the COT derives principally from the Quaternary-Holocene activity recognized on some segments, which may shed new light on its possible control on Quaternary volcanism and on the seismic hazard evaluation of the area. Field geological surveys along with kinematic analysis and numerical inversion of ∼140 new fault-slip measurements have revealed that this portion of the COT zone, previously considered a continuous, long-lived lineament, in reality has been subjected to three different kinematic regimes: 1) a Miocene transpressional phase with the maximum principal stress (σ1) chiefly trending NNE-SSW; 2) an extensional phase that started by 9 Ma, with a horizontal NW-SE-striking minimum principal stress (σ3) – permutations between σ2 and σ3 axes have been recognized at two sites – and 3) a left-lateral strike-slip phase with a horizontal ∼E-W &sigma1 and ∼N-S σ3 dating to the Late Pliocene-Quaternary. Spatially, in the Quaternary, the left-lateral component decreases toward the westernmost tip of the COT, where it transitions to extension; this produced to a N-S horst and graben structure. Hence, even if transcurrence is still active in the eastern portion of the COT, as focal mechanisms of crustal earthquakes indicate, our study demonstrates that extension is becoming the predominant structural style of deformation, at least in the western region. These major temporal and spatial changes in the tectonic regimes are attributed in part to changes in the magnitude of the boundary forces due to subduction processes. The overall orogen-perpendicular extension might be the result of vertical stress larger than both the horizontal stresses induced by gravitational effect of a thickened crust.

Tracking eolian dust with helium and thorium: Impacts of grain size and provenance

Reconstructions of the deposition rate of windblown mineral dust in ocean sediments offer an important means of tracking past climate changes and of assessing the radiative and biogeochemical impacts of dust in past climates. Dust flux estimates in ocean sediments have commonly been based on the operationally defined lithogenic fraction of sediment samples. More recently, dust fluxes have been estimated from measurements of helium and thorium, as rare isotopes of these elements (He-3 and Th-230) allow estimates of sediment flux, and the dominant isotopes (He-4 and Th-232) are uniquely associated with the lithogenic fraction of marine sediments. In order to improve the fidelity of dust flux reconstructions based on He and Th, we present a survey of He and Th concentrations in sediments from dust source areas in East Asia, Australia and South America. Our data show systematic relationships between He and Th concentrations and grain size, with He concentrations decreasing and Th concentrations increasing with decreasing grain size. We find consistent He and Th concentrations in the fine fraction (<5 μm) of samples from East Asia, Australia and Central South America (Puna-Central West Argentina), with Th concentrations averaging 14 μg/g and He concentrations averaging 2 μcc STP/g. We recommend use of these values for estimating dust fluxes in sediments where dust is dominantly fine-grained, and suggest that previous studies may have systematically overestimated Th-based dust fluxes by 30%. Source areas in Patagonia appear to have lower He and Th contents than other regions, as fine fraction concentrations average 0.8 μcc STP/g and 9 μg/g for 4He and 232Th, respectively. The impact of grain size on lithogenic He and Th concentrations should be taken into account in sediments proximal to dust sources where dust grain size may vary considerably. Our data also have important implications for the hosts of He in long-traveled dust and for the 3He/4He ratio used for terrigenous He in studies of extraterrestrial He in sediments and ice. We also investigate the use of He/Th ratios as a provenance tracer. Our results suggest differences in fine fraction He/Th ratios between East Asia, Australia, central South America and Patagonia, with ratios showing a positive relationship with the geological age of source rocks. He/Th ratios may thus provide useful provenance information, for example allowing separation of Patagonian sources from Puna-Central West Argentina or Australian dust sources. He/Th ratios in open-ocean marine sediments are similar to ratios in the fine fraction of upwind dust source areas. He/Th ratios in mid-latitude South Atlantic sediments suggest that dust in this region primarily derives from the Puna-Central West Argentina region (23–32°S) rather than Patagonia (>38°S). In the equatorial Pacific, He/Th ratios are much lower than in extratropical Pacific sediments or potential source areas measured as a part of this study (East Asia, South America, Australia) for reasons that are at present unclear, complicating their use as provenance tracers in this region.

Procedimientos de construcción del espacio en Fuego en Casabindo, de Héctor Tizón

En Fuego en Casabindo (1969), Héctor Tizón configura una imagen poética del espacio de la Puna porque pretende re-crear ese mundo afectivamente a través de su memoria. Este espacio escritural no está configurado desde una visión objetiva sino desde la afectividad del que lo vivió y amó, desde la experiencia íntima y personal. Los espacios en Fuego en Casabindo no son referenciales, sino que asumen valores afectivos, tienen gran importancia en el andamiaje constructivo del relato y determinan un tipo de lectura de la novela, la lectura poética.

Estrategias constructivas de la espacialidad en El salar de Fausto Burgos

En El Salar, novela del cielo puneño de Fausto Burgos, la descripción del espacio adquiere distintas funciones que se encuentran en relación directa con la mirada que el autor-narrador tiene sobre ese mundo. Nuestro objetivo es analizar los modos de textualización del espacio considerados, fundamentalmente, en su relación con la concepción ideológica del autor con respecto a esta región y a los hombres que la habitan. Para esto, analizaremos las funciones que adquieren los fragmentos descriptivos en el relato y su proyección en la intencionalidad del mismo. Así, advertimos, la descripción tiene valor documental, pictórico o poético entre otros, pero, en último término, son todos subsidiarios de la intención social.

Dissolved actinium in the ocean

The measurement of short-lived 223Ra often involves a second measurement for supported activities, which represents 227Ac in the sample. Here we exploit this fact, presenting a set of 284 values on the oceanic distribution of 227Ac, which was collected when analyzing water samples for short-lived radium isotopes by the radium delayed coincidence counting system. The present work compiles 227Ac data from coastal regions all over the northern hemisphere, including values from ground water, from estuaries and lagoons, and from marine end-members. Deep-sea samples from a continental slope off Puerto Rico and from an active vent site near Hawaii complete the overview of 227Ac near its potential sources. The average 227Ac activities of nearshore marine end-members range from 0.4 dpm/m**3 at the Gulf of Mexico to 3.0 dpm m? 3 in the coastal waters of the Korean Strait. In analogy to 228Ra, we find the extension of adjacent shelf regions to play a substantial role for 227Ac activities, although less pronounced than for radium, due to its weaker shelf source. Based on previously published values, we calculate an open ocean 227Ac inventory of 1.35 * 1018 dpm 227Acex in the ocean, which corresponds to 37 moles, or 8.4 kg. This implies a flux of 127 dpm/m**2/y from the deep-sea floor. For the shelf regions, we obtain a global inventory of 227Ac of 4.5 * 10**15 dpm, which cannot be converted directly into a flux value, as the regional loss term of 227Ac to the open ocean would have to be included. Ac has so far been considered to behave similarly to Ra in the marine environment, with the exception of a strong Ac source in the deep-sea due to 231Paex. Here, we present evidence of geochemical differences between Ac, which is retained in a warm vent system, and Ra, which is readily released [Moore, W.S., Ussler, W. and Paull, C.K., 2008-this issue. Short-lived radium isotopes in the Hawaiian margin: Evidence for large fluid fluxes through the Puna Ridge. Marine Chemistry]. Another potential mechanism of producing deviations in 227Ac/228Ra and daughter isotope ratios from the expected production value of lithogenic material is observed at reducing environments, where enrichment in uranium may occur. The presented data here may serve as a reference for including 227Ac in circulation models, and the overview provides values for some end-members that contribute to the global Ac distribution.

Violencia e invisibilidad indígena : La cuestión de los pueblos originarios durante el primer peronismo

El presente trabajo busca profundizar en el análisis de los vínculos existentes entre el primer gobierno peronista y la cuestión indígena, centrándose en las políticas gubernamentales desarrolladas por el gobierno de Perón frente a dos fuertes conflictos violentos que tuvieron lugar entre 1946 y 1947: el "Malón de la paz", la movilización indígena llevada a cabo entre mayo y agosto de 1947, cuando 174 kollas caminaron 2000 kilómetros desde la Puna y el valle de Orán hasta la Capital Federal para reclamar por la titularidad de sus tierras, en manos de terratenientes y en denuncia de las condiciones de explotación en las que trabajaban; y "Masacre de Rincón Bomba", el conflicto desarrollado en una pequeña localidad de Formosa, cuando indígenas de comunidades wichi, tobas y principalmente pilagás fueron masacradas por la Gendarmería Nacional en un confuso episodio, que sale a la luz hace pocos años. El objetivo en ambos puntos es doble: por un lado analizar la relación entre los intereses e intenciones del gobierno de Juan Domingo Perón para con las comunidades originarias, visibilizando su existencia y sus condiciones de vida en tanto sujetos de derechos históricamente vulnerados. Por otro, abrir el debate historiográfico sobre el quehacer de los historiadores respecto de una temática que ha sido silenciada durante décadas, negando la existencia y la identidad de los pueblos originarios

Violencia e invisibilidad indígena : La cuestión de los pueblos originarios durante el primer peronismo

El presente trabajo busca profundizar en el análisis de los vínculos existentes entre el primer gobierno peronista y la cuestión indígena, centrándose en las políticas gubernamentales desarrolladas por el gobierno de Perón frente a dos fuertes conflictos violentos que tuvieron lugar entre 1946 y 1947: el "Malón de la paz", la movilización indígena llevada a cabo entre mayo y agosto de 1947, cuando 174 kollas caminaron 2000 kilómetros desde la Puna y el valle de Orán hasta la Capital Federal para reclamar por la titularidad de sus tierras, en manos de terratenientes y en denuncia de las condiciones de explotación en las que trabajaban; y "Masacre de Rincón Bomba", el conflicto desarrollado en una pequeña localidad de Formosa, cuando indígenas de comunidades wichi, tobas y principalmente pilagás fueron masacradas por la Gendarmería Nacional en un confuso episodio, que sale a la luz hace pocos años. El objetivo en ambos puntos es doble: por un lado analizar la relación entre los intereses e intenciones del gobierno de Juan Domingo Perón para con las comunidades originarias, visibilizando su existencia y sus condiciones de vida en tanto sujetos de derechos históricamente vulnerados. Por otro, abrir el debate historiográfico sobre el quehacer de los historiadores respecto de una temática que ha sido silenciada durante décadas, negando la existencia y la identidad de los pueblos originarios

Violencia e invisibilidad indígena : La cuestión de los pueblos originarios durante el primer peronismo

El presente trabajo busca profundizar en el análisis de los vínculos existentes entre el primer gobierno peronista y la cuestión indígena, centrándose en las políticas gubernamentales desarrolladas por el gobierno de Perón frente a dos fuertes conflictos violentos que tuvieron lugar entre 1946 y 1947: el "Malón de la paz", la movilización indígena llevada a cabo entre mayo y agosto de 1947, cuando 174 kollas caminaron 2000 kilómetros desde la Puna y el valle de Orán hasta la Capital Federal para reclamar por la titularidad de sus tierras, en manos de terratenientes y en denuncia de las condiciones de explotación en las que trabajaban; y "Masacre de Rincón Bomba", el conflicto desarrollado en una pequeña localidad de Formosa, cuando indígenas de comunidades wichi, tobas y principalmente pilagás fueron masacradas por la Gendarmería Nacional en un confuso episodio, que sale a la luz hace pocos años. El objetivo en ambos puntos es doble: por un lado analizar la relación entre los intereses e intenciones del gobierno de Juan Domingo Perón para con las comunidades originarias, visibilizando su existencia y sus condiciones de vida en tanto sujetos de derechos históricamente vulnerados. Por otro, abrir el debate historiográfico sobre el quehacer de los historiadores respecto de una temática que ha sido silenciada durante décadas, negando la existencia y la identidad de los pueblos originarios

Volcanic setting of the Bajo de la Alumbrera porphyry Cu-Au deposit, Farallon Negro Volcanics, Northwest Argentina

The late Miocene Farallon Negro volcanics, comprising basaltic to rhyodacitic volcano-sedimentary rocks, host the Bajo de la Alumbrera porphyry copper-gold deposit in northwest Argentina. Early studies of the geology of the district have underpinned the general model for porphyry ore deposits where hydrothermal alteration and mineralization develop in and around porphyritic intrusions emplaced at shallow depths (2.5-3.5 km) into stratovolcanic assemblages. The Farallon Negro succession is dominated by thick sequences of volcano-sedimentary breccias, with lavas forming a minor component volumetrically. These volcaniclastic rocks conformably overlie crystalline basement-derived sedimentary rocks deposited in a developing foreland basin southeast of the Puna-Altiplano plateau. Within the Farallon Negro volcanics, volcanogenic accumulations evolved from early mafic to intermediate and silicic compositions. The younger and more silicic rocks are demonstrably coeval and comagmatic with the earliest group of mineralized porphyritic intrusions at Bajo de la Alumbrera. Our analysis of the volcanic stratigraphy and facies architecture of the Farallon Negro volcanics indicates that volcanic eruptions evolved from effusive to mixed effusive and explosive styles, as magma compositions changed to more intermediate and silicic compositions. Air early phase of mafic to intermediate voleanism was characterized by small synsedimentary intrusions with peperitic contacts, and lesser lava units scattered widely throughout the district, and interbedded with thick and extensive successions of coarse-grained sedimentary breccias. These sedimentary breccias formed from numerous debris- and hyperconcentrated flow events. A later phase of silicic volcanism included both effusive eruptions, forming several areally restricted lavas, and explosive eruptions, producing more widely dispersed (up to 5 kin) tuff units, some tip to 30-m thickness in proximal sections. Four key features of the volcanic stratigraphy suggest that the Farallon Negro volcanics need not simply record the construction of a large steep-sided polygenetic stratovolcano: (1) sheetlike, laterally continuous debris-flow and other coarse-grained sedimentary deposits are dominant, particularly in the lower sections; (2) mafic-intermediate composition lavas are volumetrically minor; (3) peperites are present throughout the sequence; and (4) fine-grained lacustrine sandstone-siltstone sequences occur in areas previously thought to be proximal to the summit region of the stratovolcano. Instead, the nature, distribution, and geometry of volcanic and volcaniclastic facies suggest that volcanism occurred as a relatively low relief, multiple-vent volcanic complex at the eastern edge of a broad, > 200-km-wide late Miocene volcanic belt and oil ail active foreland sedimentary basin to the Puna-Altiplano. Volcanism that occurred synchronously with the earliest stages of porphyry-related mineralization at Bajo de la Alumbrera apparently developed in an alluvial to ring plain setting that was distal to larger volcanic edifices.

GIS technologies and spatial organization patterns among hunter-gatherers: an archaeological case study from Southern Patagonia (southern South America)

This paper discusses some aspects of hunter-gatherer spatial organization in southern South Patagonia, in later times to 10,000 cal yr BP. Various methods of spatial analysis, elaborated with a Geographic Information System (GIS) were applied to the distributional pattern of archaeological sites with radiocarbon dates. The shift in the distributional pattern of chronological information was assessed in conjunction with other lines of evidence within a biogeographic framework. Accordingly, the varying degrees of occupation and integration of coastal and interior spaces in human spatial organization are explained in association with the adaptive strategies hunter-gatherers have used over time. Both are part of the same human response to changes in risk and uncertainty variability in the region in terms of resource availability and environmental dynamics.

Motivating residents to combat invasive species on private lands: social norms and community reciprocity

Invasive species (IS) threaten biodiversity and ecosystem functioning. To achieve landscape-scale reductions in IS and the associated gains for biodiversity, IS control efforts must be expanded across private lands. Enhancing IS control across private lands requires an understanding of the factors that motivate residents to engage or prohibit residents from engaging in efforts to control IS. Drawing from the collective interest model and literature, we sought to understand how a wide range of interpersonal, intrapersonal, and contextual factors might influence resident action around combating the invasive tree albizia (Falcataria moluccana), in the Puna District of Hawaiʻi. To do so, we used a cross-sectional survey of 243 residents and elastic net regression techniques. We found that residents’ actions related to IS control were related to their perceptions of social norms and community reciprocity regarding albizia control, as well as their knowledge of effective control strategies and their risk perceptions regarding albizia. These findings suggest that, although common intervention approaches that focus on providing education or subsidies are important, they may be more effective at reducing the spread of IS if coupled with approaches that build community reciprocity and norms.