37 results on '"González-García, Diego"'
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2. Bubble-enhanced basanite–tephrite mixing in the early stages of the Cumbre Vieja 2021 eruption, La Palma, Canary Islands
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González-García, Diego, Boulesteix, Thomas, Klügel, Andreas, and Holtz, François
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- 2023
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3. Diffusive exchange of trace elements between alkaline melts: implications for element fractionation and timescale estimations during magma mixing
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González-García, Diego, Petrelli, Maurizio, Behrens, Harald, Vetere, Francesco, Fischer, Lennart A., Morgavi, Daniele, and Perugini, Diego
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Physics - Geophysics - Abstract
The diffusive exchange of 30 trace elements during the interaction of natural mafic and silicic alkaline melts was experimentally studied at conditions relevant to shallow magmatic systems. In detail, a set of 12 diffusion couple experiments have been performed between natural shoshonitic and rhyolitic melts from the Vulcano Island (Aeolian archipelago, Italy) at a temperature of 1200 {\deg}C, pressures from 50 to 500 MPa, and water contents ranging from nominally dry to ca. 2 wt. %. Concentration-distance profiles, measured by Laser Ablation ICP-MS, highlight different behaviours, and trace elements were divided into two groups: (1) elements with normal diffusion profiles (13 elements, mainly low field strength and transition elements), and (2) elements showing uphill diffusion (17 elements including Y, Zr, Nb, Pb and rare earth elements, except Eu). For the elements showing normal diffusion profiles, chemical diffusion coefficients were estimated using a concentration-dependent evaluation method, and values are given at four intermediate compositions (SiO2 equal to 58, 62, 66 and 70 wt. %, respectively). A general coupling of diffusion coefficients to silica diffusivity is observed, and variations in systematics are observed between mafic and silicic compositions. Results show that water plays a decisive role on diffusive rates in the studied conditions, producing an enhancement between 0.4 and 0.7 log units per 1 wt.% of added H2O. Particularly notable is the behaviour of the trivalent-only REEs (La to Nd and Gd to Lu), with strong uphill diffusion minima, diminishing from light to heavy REEs. Modelling of REE profiles by a modified effective binary diffusion model indicates that activity gradients induced by the SiO2 concentration contrast are responsible for their development, inducing a transient partitioning of REEs towards the shoshonitic melt., Comment: 57 pages, 12 figures, 5 tables
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- 2018
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4. Exponential Decay Of Concentration Variance During Magma Mixing: Robustness Of A Volcanic Chronometer And Implications For The Homogenization Of Chemical Heterogeneities In Magmatic Systems
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Rossi, Stefano, Petrelli, Maurizio, Morgavi, Daniele, González-García, Diego, Fischer, Lennart A., Vetere, Francesco, and Perugini, Diego
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Physics - Geophysics - Abstract
The mixing of magmas is a fundamental process in the Earth system causing extreme compositional variations in igneous rocks. This process can develop with different intensities both in space and time, making the interpretation of compositional patterns in igneous rocks a petrological challenge. As a time-dependent process, magma mixing has been suggested to preserve information about the time elapsed between the injection of a new magma into sub-volcanic magma chambers and eruptions. This allowed the use of magma mixing as an additional volcanological tool to infer the mixing-to-eruption timescales. In spite of the potential of magma mixing processes to provide information about the timing of volcanic eruptions its statistical robustness is not yet established. This represents a prerequisite to apply reliably this conceptual model. Here, new chaotic magma mixing experiments were performed at different times using natural melts. The degree of reproducibility of experimental results was tested repeating one experiment at the same starting conditions and comparing the compositional variability. We further tested the robustness of the statistical analysis by randomly removing from the analysed dataset a progressively increasing number of samples. Results highlight the robustness of the method to derive empirical relationships linking the efficiency of chemical exchanges and mixing time. These empirical relationships remain valid by removing up to 80% of the analytical determinations. Experimental results were applied to constrain the homogenization time of chemical heterogeneities in natural magmatic system during mixing. The calculations show that, when the mixing dynamics generate millimetre thick filaments, homogenization timescales of the order of a few minutes are to be expected.
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- 2017
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5. Water-enhanced interdiffusion of major elements between natural shoshonite and high-K rhyolite melts
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González-García, Diego, Behrens, Harald, Petrelli, Maurizio, Vetere, Francesco, Morgavi, Daniele, Zhang, Chao, and Perugini, Diego
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Physics - Geophysics - Abstract
The interdiffusion of six major elements (Si, Ti, Fe, Mg, Ca, K) between natural shoshonite and a high-K calc-alkaline rhyolite (Vulcano island, Aeolian archipelago, Italy) has been experimentally measured by the diffusion couple technique at 1200{\deg}C, pressures from 50 to 500 MPa and water contents from 0.3 (nominally dry) to 2 wt%. The experiments were carried out in an internally heated pressure vessel, and major element profiles were later acquired by electron probe microanalysis. The concentration-distance profiles are evaluated using a concentration-dependent diffusivity approach. Effective binary diffusion coefficients for four intermediate silica contents are obtained by the Sauer-Freise modified Boltzmann-Matano method. At the experimental temperature and pressures, the diffusivity of all studied elements notably increases with dissolved H2O content. Particularly, diffusion is up to 1.4 orders of magnitude faster in a melt containing 2 wt.% H2O than in nominally dry melts. This effect is slightly enhanced in the more mafic compositions. Uphill diffusion was observed for Al, while all other elements can be described by the concept of effective binary interdiffusion. Ti is the slowest diffusing element through all experimental conditions and compositions, followed by Si. Fe, Mg, Ca and K diffuse at similar rates but always more rapidly than Si and Ti. This trend suggests a strong coupling between melt components. Since effects of composition (including water content) are dominant, a pressure effect on diffusion cannot be clearly resolved in the experimental pressure range.
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- 2017
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6. Chemical interdiffusion between Na-series tephritic and phonolitic melts with different H2O content, temperature, and oxygen fugacity values
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González García, Diego, Pohl, Florian, Marxer, Felix, Krasheninnikov, Stepan, Almeev, Renat, Holtz, François, González García, Diego, Pohl, Florian, Marxer, Felix, Krasheninnikov, Stepan, Almeev, Renat, and Holtz, François
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The diffusive exchange of major elements in Na-series tephrite–phonolite diffusion couples with compositions relevant to the Canary Islands magmatism was determined at 300 MPa and variable H2O concentrations (0.3 wt % to 3.3 wt %), temperatures (1150 to 1300 °C), and fO2 levels (NNO−1.5 to NNO+1.7). Composition-dependent effective binary diffusion coefficients were determined from concentration–distance profiles. Results show a wide range of diffusivities for different cations, consistently following the sequence Na ≫ Al ≫ K ≥ Mg = Fe = Ca > Si > Ti, with a mild diffusivity contrast (0.2–0.8 log units) between tephritic and phonolitic melts. Na is the fastest component, with diffusivities falling ∼1.0 log units above those of Si for any given condition. An anomalously fast Al diffusion is observed, with DAl falling ∼0.4 log units above Si and ∼0.6 log units below Na, suggesting a prevalence of Al–alkali coupling across our range of run conditions. The relationships between log D and H2O content in melt for all cations in an intermediate composition are strongly nonlinear and can be fitted using an exponential function with a convergence in diffusion coefficients for different temperatures with increasing H2O content. Thus, Arrhenius analyses result in a decrease in activation energies from 222–293 kJ mol−1 at 1.7 wt % H2O to 48–112 kJ mol−1 at 3.0 wt % H2O. These results provide new data on chemical interdiffusion in highly alkaline Na-rich melts and suggest that H2O content plays a key role in increasing the chemical efficiency of magma mixing at low temperatures. The obtained dataset is used to test chemical controls of magma mixing in the El Abrigo ignimbrite, Tenerife, where banded pumices involving basanitic–tephritic to phonolitic magmas are common in several compositionally bimodal ignimbrite units., Alexander von Humboldt Stiftung, Deutsche Forschungsgemeinschaft, Depto. de Mineralogía y Petrología, Fac. de Ciencias Geológicas, TRUE, pub
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- 2024
7. A Raman spectroscopic tool to estimate chemical composition of natural volcanic glasses
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González-García, Diego, Giordano, Daniele, Russell, James K., and Dingwell, Donald B.
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- 2020
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8. La digitalización de la vida contemporánea: el saber, el poder y la subjetivación como vías de acceso a la experiencia digital
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Maureira, Marco, González García, Diego, Maureira, Marco, and González García, Diego
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This work argues that one of the fundamental characteristics that define our contemporary age is the digitization of life. To explain this digitization process, we will use a conceptual device of great importance in the last period of Foucault’s intellectual production: experience. We will argue that the digital experience to which we are confronted nowadays —for example, in the advent of biometrics— is defined by the interaction of three simultaneous dimensions: a knowledge formation matrix (cybernetic-digital), a behavior standardization matrix (executed as algorithmic governmentality) and a matrix for subjectivation processes, in which the contemporary subject is paradoxically questioned for being more and less than an individual. Furthermore, we incorporate the notion of mode of existence of the technical object developed by Gilbert Simondon, to conclude that technology can become a fourth way of access to the digital experience that characterizes the evolution of our societies., En este trabajo se sostiene que una de las características fundamentales que define nuestra época contemporánea es la denominada digitalización de la vida. Para explicar en qué consiste este proceso, utilizaremos un dispositivo conceptual de gran importancia en el último periodo de producción intelectual de Foucault; a saber, el concepto de experiencia. En este sentido, sostendremos que la experiencia digital a la que nos enfrentamos hoy en día —por ejemplo, en el advenimiento de la biometría— implica la ejecución simultánea y entrelazada de una matriz para la formación de los saberes (de tipo cibernético-digital), de una matriz para normativizar el comportamiento (ejecutada como gubernamentalidad algorítmica) y de una matriz para la puesta en juego de los procesos de subjetivación, en que el sujeto contemporáneo es paradójicamente interpelado a ser más y menos que un individuo. Además, incorporando la noción de modo de existencia del objeto técnico desarrollada por Gilbert Simondon, concluiremos que la tecnología se puede convertir en una cuarta vía de acceso a la experiencia digital que caracteriza el devenir de nuestro tiempo.
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- 2023
9. Bubble-enhanced basanite–tephrite mixing in the early stages of the Cumbre Vieja 2021 eruption, La Palma, Canary Islands
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Alexander von Humboldt Foundation, University of Bremen, German Research Foundation, González-García, Diego, Boulesteix, Thomas, Klügel, Andreas, Holtz, François, Alexander von Humboldt Foundation, University of Bremen, German Research Foundation, González-García, Diego, Boulesteix, Thomas, Klügel, Andreas, and Holtz, François
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Syneruptive magma mixing is widespread in volcanic eruptions, affecting explosivity and composition of products, but its evidence in basaltic systems is usually cryptic. Here we report direct evidence of mixing between basanitic and tephritic magmas in the first days of the 2021 Tajogaite eruption of Cumbre Vieja, La Palma. Groundmass glass in tephritic tephra from the fifth day of the eruption is locally inhomogeneous, showing micron-scale filamentary structures of Si-poor and Fe-, Mg-rich melt, forming complex filaments attached to bubbles. Their compositional distribution attests the presence of primitive basanitic magma, with compositions similar to late-erupted melts, interacting with an evolved tephritic melt during the first week of the event. From filament morphology, we suggest their generation by dragging and folding of basanitic melt during bubble migration through melt interfaces. Semi-quantitative diffusion modelling indicates that the filamentary structures are short-lived, dissipating in timescales of tens of seconds. In combination with thermobarometric constraints, we suggest a mixing onset by sub-Moho remobilization of a tephritic reservoir by basanite input, followed by turbulent ascent of a mingled magma. In the shallow conduit or lava fountain, bubble nucleation and migration triggered further mingling of the distinct melt-phases. This phenomenon might have enhanced the explosive behaviour of the eruption in such period, where violent strombolian explosions were common.
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- 2023
10. La digitalización de la vida contemporánea: el saber, el poder y la subjetivación como vías de acceso a la experiencia digital
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Maureira-Velásquez, Marco, primary and González-García, Diego, additional
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- 2023
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11. Evidence of bubble-assisted magma mixing in the early stage of the Cumbre Vieja 2021 eruption, La Palma, Canary Islands
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González-García, Diego, primary, Boulesteix, Thomas, additional, Klügel, Andreas, additional, and Holtz, Francois, additional
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- 2023
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12. Los ecos del superhombre: ciborgs, posthumanos y sujetos contemporáneos
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González-García, Diego, primary and Maureira-Velásquez, Marco, additional
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- 2022
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13. Pre-eruptive conditions and dynamics recorded in banded pumices from the El Abrigo caldera-forming eruption (Tenerife, Canary Islands)
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Martí Molist, Joan [0000-0003-3930-8603], González-García, Diego, Petrelli, Mauricio, Perugini, D., Giordano, Daniele, Vasseur, J., Paredes-Mariño, Joali, Martí Molist, Joan, Dingwell, Donald Bruce, Martí Molist, Joan [0000-0003-3930-8603], González-García, Diego, Petrelli, Mauricio, Perugini, D., Giordano, Daniele, Vasseur, J., Paredes-Mariño, Joali, Martí Molist, Joan, and Dingwell, Donald Bruce
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The El Abrigo member of the Diego Hernández Formation (Tenerife, Canary Islands) represents the final (170 ka) and most voluminous eruption (>20 km3 DRE) of the last cycle of explosive activity of the Las Cañadas volcano. It is a dominantly phonolitic ignimbrite containing both mafic and banded pumices, suggesting that magma mixing played an important role in triggering the eruption and modulating eruptive dynamics. Here we use petrology, together with glass and mineral geochemistry of enclave-rich mafic scoriae, banded and phonolitic pumices from El Abrigo ignimbrite, to shed light on the pre-eruptive storage conditions and processes governing magma ascent and interaction dynamics and to provide a first-order assessment of the contribution of magma mixing and crystal mush melting to the dynamics of this eruptive event. The distribution of major elements in glasses is consistent with diffusive exchange between the interacting melts whereby Na transfers from the phonolite to the tephriphonolitic melt. However, V, Zr, Ba and Eu suggest a complex scenario in which an intruding tephritic to phonotephritic magma interacted with two distinct zones of a phonolitic magma chamber, one occupied by a crystal rich, low-Zr and high Ba phonolite, and the other by an evolved, crystal poor, high-Zr phonolite. These results, coupled with mineral-melt thermobarometry, allow us to reconstruct the Las Cañadas plumbing system at the end of the Diego Hernández cycle, and to evaluate the contribution of cumulate mush melting and magma mixing in as follows: (1) the parental tephritic magma was stored at or near the Moho (410-450 MPa) at 1050°C where it was periodically replenished by more primitive basanitic magma; (2) upon ascent, the tephrite intruded into a shallow and zoned phonolitic storage system, triggering the disruption of a crystal mush in its base, and (3) subsequently interacted with a crystal-poor zone within the reservoir. Energy balance evaluations suggest that relative maf
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- 2022
14. Chemical interdiffusion in Na-rich alkaline melts: insights from tephrite-phonolite couple experiments
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González-García, Diego, Pohl, Florian, Krasheninnikov, Stepan P., Beckmann, Philipp, Behrens, Harald, and Holtz, François
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Although alkaline melts represent an important fraction of the magmatism in ocean islands, there is a lack of chemical diffusion data in such compositions. We present here the result of a series of interdiffusion experiments using natural tephritic and phonolitic melts from the Canary Islands as endmembers. Experiments were run in two internally heated pressure vessels at a pressure of 300 MPa, temperatures from 1150 to 1300°C, oxygen fugacity from NNO to approx. NNO+3, and water contents between 0.3 and 3.3 wt.%. Major element concentration-distance profiles were measured by electron microprobe and effective binary diffusion coefficients (D) were obtained by a modified Boltzmann-Matano analysis. Results show a wide range of diffusivities for different cations, following the sequence Na >> Al > K Mg = Fe = Ca > Si > Ti. Na diffusivities are the fastest and are consistently 1 log unit above those of Si for a given experiment. Al diffusion is remarkably fast, falling ca. 0.4 log units above Si, an effect not observed before in diffusion studies. The relationships between log D and H2O content in melt for all cations are strongly non-linear and can be fitted by using an exponential function, with an apparent convergence in diffusion coefficients towards the water-rich end. Our results provide new data on chemical interdiffusion in Na-rich, highly alkaline melts and allow to test chemical controls of magma mixing in Tenerife, where banded pumices are common in several bimodal ignimbritic units.
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- 2022
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15. La digitalización de la vida y la emergencia de nuevas formas de subjetivación
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González García, Diego and Tirado Serrano, Francisco Javier
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Digitalització de la vida ,Subjectivació ,Subjetivación ,Ciències Humanes ,Filosofía de la técnica ,Subjectivation ,Digitalización de la vida ,Digitalisation of life ,Philosophy of technology ,Filosofia de la tècnica - Abstract
La tesi indaga el fenomen contemporani que anomenem experiència digital o digitalització de la vida. Aquest fenomen està donat per la disseminació i expansió de les tecnologies digitals a la vida quotidiana. El treball analitza quatre qüestions principals que constitueixen l'experiència digital contemporània: 1- el naixement d'una manera de saber matritzada per les ciències cibernètiques, 2- una nova forma d'exercici del poder donat pel desenvolupament de tecnologies de govern algorísmiques, 3- un manera de subjectivar-se on l'individu clàssic es posa en qüestió a partir de la producció de dades i els subjectes humans són cridats a ser, alhora més i menys que individus, i 4- la immensa producció d'objectes digitals (dades, algorismes, plataformes ) que s'alimenten i existeixen gràcies a les conductes humanes. Des d'aquesta perspectiva d'anàlisi s'indaguen les pràctiques concretes del moviment Quantified Self, que a partir de l'ús de les tecnologies digitals del self-tracking constitueixen un dels retrats del fenomen de la digitalització de la vida. Finalment, la tesi suggereix la discussió d'un nou ascetisme consubstanciat amb les tecnologies, així ens podrem acostar a una reflexió crítica que redirigeixi el problema de la tècnica capitalista cap a altres camins que avizorin un món i no el col·lapse imminent. La tesis indaga el fenómeno contemporáneo que denominamos experiencia digital o digitalización de la vida. Este fenómeno está dado por la diseminación y expansión de las tecnologías digitales en la vida cotidiana. El trabajo analiza cuatro cuestiones principales que constituyen la experiencia digital contemporánea: 1- el nacimiento de un forma de saber matrizada por las ciencias cibernéticas, 2- una novedosa forma de ejercicio del poder dado por el desarrollo de tecnologías de gobierno algorítmicas, 3- un modo de subjetivarse donde el individuo clásico se pone en cuestión a partir de la producción de datos y los sujetos humanos son llamados a ser, la vez más y menos que individuos, y 4- la inmensa producción de objetos digitales (datos, algoritmos, plataformas) que se alimentan y existen gracias a las conductas humanas. Desde esta perspectiva de análisis se indagan las prácticas concretas del movimiento Quantified Self, quienes a partir del uso de las tecnologías digitales del self-tracking constituyen uno de los retratos del fenómeno de la digitalización de la vida. Por último, la tesis sugiere la discusión de un nuevo ascetismo consustanciado con las tecnologías, de este modo, nos podremos acercar a una reflexión crítica que redirija el problema de la técnica capitalista hacia otros caminos que avizoren un mundo y no el colapso inminente. The thesis explores the contemporary phenomenon that we refer to as the digital experience or digitalisation of life. This phenomenon is the result of the dissemination and expansion of digital technologies in everyday life. The study analyses four main issues that constitute the contemporary digital experience: 1- the birth of a form of knowledge matrixed by cybernetic sciences, 2- a new form of exercise of power given by the development of algorithmic governance technologies, 3- a way of subjectivation where the classical individual is questioned by the production of data and human subjects are called to be both more and less than individuals, and 4- the immense production of digital objects (data, algorithms, platforms) that are fed and exist thanks to human behaviours. From this perspective of analysis, we explore the concrete practices of the Quantified Self movement, who, through the use of digital self-tracking technologies, constitute one of the portraits of the phenomenon of the digitalisation of life. Finally, the thesis suggests the discussion of a new asceticism consubstantiated with technologies, in this way, we will approach a critical reflection that redirects the problem of the capitalist technique towards other paths that provide a world and not the imminent collapse.
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- 2022
16. Pre-Eruptive Conditions and Dynamics Recorded in Banded Pumices from the El Abrigo Caldera-Forming Eruption (Tenerife, Canary Islands)
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González-García, Diego, primary, Petrelli, Maurizio, additional, Perugini, Diego, additional, Giordano, Daniele, additional, Vasseur, Jérémie, additional, Paredes-Mariño, Joali, additional, Marti, Joan, additional, and Dingwell, Donald B, additional
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- 2022
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17. Pre-eruptive magma hybridization and storage conditions recorded in banded pumices from the caldera-forming El Abrigo eruption (Tenerife)
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González-García, Diego, Petrelli, Mauricio, Perugini, D., Paredes-Mariño, Joali, Martí Molist, Joan, Vasseur, J., and Dingwell, Donald Bruce
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El Abrigo ,Tenerife ,Eruption ,Magmatism - Abstract
The El Abrigo member, belonging to the Diego Hernández Formation (Tenerife, Canary Islands), represents the final (0.179 Ma) and most voluminous eruption (>20 km3 DRE) of the last cycle of explosive volcanism of the Las Cañadas volcano. Its products are predominantly phonolitic, but both mafic scoriae and banded pumices are commonly found, suggesting that El Abrigo eruption was triggered via the input of fresh, more mafic magma into a shallow, phonolitic magma chamber. A petrological and geochemical study was carried out on a variety of pumices sampled in the El Abrigo member, ranging from dominantly mafic to banded, and in turn to phonolitic. Banded pumices show a diversity of textures varying from coarsely to finely banded. Mafic scoriae host numerous phonolitic enclaves, sometimes grading to banded within a hand sample. In contrast, phonolitic pumices are homogeneous, almost crystal-free and highly vesicular. Small-scale, fluidal mixing structures are widely present in SEM BSE images and involve the entire compositional spectrum from a partially-crystallized tephriphonolitic composition (SiO2 ~52 wt.%; MgO ~3 wt.%) to a phonolitic melt (SiO2 ~61 wt.%; MgO ~0.3 wt.%). The distribution of fast-diffusing versus slow-diffusing elements indicates that diffusive hybridization has played a significant role. The presence of such small-scale structures and high compositional gradients at scales in the order of tens to hundreds of microns suggest that mixing was of limited efficiency and that the eruption likely started shortly after the beginning of this process, as longer timescales would erase such heterogeneities by advection and chemical diffusion. Several mineral and mineral-melt thermobarometric methods show good agreement and suggest that the mafic end-member had a tephritic composition and was stored prior to the mixing event at ~400 MPa (lowermost oceanic crust) and 1050ºC, and both endmembers contained ~3 wt.% dissolved H2O.
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- 2020
18. Raman Spectroscopy from Laboratory and Proximal to Remote Sensing: A Tool for the Volcanological Sciences
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Giordano, Daniele, primary, Russell, James K., additional, González-García, Diego, additional, Bersani, Danilo, additional, Dingwell, Donald B., additional, and Del Negro, Ciro, additional
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- 2020
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19. Magma hybridization recorded in banded pumices from the 0.17 Ma El Abrigo eruption, Tenerife: preliminary results
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González-García, Diego, Perugini, D., Giordano, Daniele, Vasseur, J., Martí Molist, Joan, and Dingwell, Donald Bruce
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volcanology ,Canary Islands - Abstract
Goldschmidt 2019 in Barcelona, Spain, 18-23 august 2019, The El Abrigo member, belonging to the Diego Hernández Formation (SE Tenerife, Canary Islands) represents the final (0.17 Ma) and most voluminous eruption (>20 km3 DRE) of the last cycle of explosive eruptions of the Las Cañadas volcano. It is a dominantly phonolitic ignimbrite, but both mafic and banded pumices are common. It has been suggested that the El Abrigo eruption was triggered via the input of fresh, more mafic magma into a shallow, phonolitic magma chamber. Here we show the first results of a petrological and geochemical study carried out on a variety of pumices sampled in the El Abrigo member, ranging from dominantly mafic to banded to phonolitic. Banded pumices show textures varying from coarsely to finely banded. More disorganized, patchy pumices are also present. Mafic pumices host numerous phonolitic enclaves, sometimes grading to banded within a hand sample. In contrast, phonolitic pumices are homogeneous, and highly vesicular. Raman spectra indicate that phonolitic glasses from both white and banded pumices contain 2.2-3.3 wt.% H2O. Small-scale, fluidal mixing structures are widely present in SEM BSE images and involve a less-evolved, partiallycrystallized melt of tephriphonolitic composition (SiO2~53 wt.%; MgO~2 wt.%) and a phonolitic melt (SiO2 ~61 wt.%; MgO ~0.3 wt.%). EPMA glass profiles highlight that the entire range of compositions is present within a single thin section, and high compositional contrasts exists on scales of tens to hundreds of microns. The presence of such small-scale structures suggest that mixing was of limited efficiency and that the eruption likely started shortly after the beginning of this process, as longer timescales would erase such heterogeneities by advection and chemical diffusion.
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- 2019
20. Interdiffusion of major elements at 1 atmosphere between natural shoshonitic and rhyolitic melts
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González-García, Diego, primary, Vetere, Francesco, additional, Behrens, Harald, additional, Petrelli, Maurizio, additional, Morgavi, Daniele, additional, and Perugini, Diego, additional
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- 2019
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21. A calibrated database of Raman spectra for natural silicate glasses: implications for modelling melt physical properties
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Giordano, Daniele, primary, González‐García, Diego, additional, Russell, James K., additional, Raneri, Simona, additional, Bersani, Danilo, additional, Fornasini, Laura, additional, Di Genova, Danilo, additional, Ferrando, Simona, additional, Kaliwoda, Melanie, additional, Lottici, Pier Paolo, additional, Smit, Matthijs, additional, and Dingwell, Donald B., additional
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- 2019
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22. Definir para gobernar:: políticas dirigidas a niños, niñas y adolescentes en situación de calle en Uruguay
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Fagundez D'Anello, Daniel A., González García, Diego, Fagundez D'Anello, Daniel A., and González García, Diego
- Abstract
This article presents the results of a study implemented in the city of Montevideo on how government policies define the subject that receives assistance, the target population for social policies for street children is constructed. After studying the policies developed for this population, the strategies and techniques for managing the problem are analyzed through work of the people that guide the policies as well as staff that provide direct assistance in the territory. Using a qualitative methodological approach, social cartography with participant observation techniques and semi-guided interviews were carried out. The authors conclude that the definition of the subject that receives assistance is the result of a constant and unfinished process that involves a series of heterogeneous elements that more people need to know about., Este artigo apresenta os resultados de um estudo realizado na cidade de Montevidéu, sobre como é construída as noções de sujeito de atendimento das políticas dirigidas a crianças e adolescentes em uma situação de rua. A partir dos estudos de governabilidade, são analisadas as estratégias e técnicas de gestão do problema, a partir da visão das posições de direção das políticas e dos trabalhadores de um projeto que realiza a atenção direta no territorio. Seguindo uma abordagem metodológica qualitativa realiza-se uma cartografia social, utilizando técnicas de observação participante e entrevistas semi-direcionadas. Concluímos que a definição do sujeito é o resultado de um processo constante e inacabado, envolvendo uma série de elementos heterogêneos que devem ser visíveis, Este artículo presenta resultados de un estudio realizado en la ciudad de Montevideo, acerca de cómo se construye la noción de sujeto de atención en las políticas dirigidas a niños, niñas y adolescentes en situación de calle. A partir de los estudios de gubernamentalidad se analizan las estrategias y técnicas de gestión del problema, desde la visión de los cargos de dirección de las políticas y de trabajadores de un proyecto que realiza la atención directa en territorio. Siguiendo un enfoque metodológico cualitativo se realiza una cartografía social con técnicas de observación participante y entrevistas semi-dirigidas. Concluimos que la definición del sujeto es el resultado de un proceso constante e inacabado, en donde intervienen una serie de elementos heterogéneos que es necesario hacer visibles.
- Published
- 2018
23. Pérdida de la patria potestad, adopción y consecuencias de la misma
- Author
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González García, Diego, Colina Garea, Rafael, and Universidade da Coruña. Facultade de Dereito
- Subjects
Adopción ,Patria potestad ,Violencia familiar ,Desamparo - Abstract
Traballo fin de grao (UDC.DER). Dereito. Curso 2016/2017
- Published
- 2017
24. El gobierno de la niñez y la adolescencia en situación de calle : un estudio de la racionalidad de las políticas sociales focalizadas
- Author
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González García, Diego, Chavez Bidart, Jorge, Di Martino Bermudez, Mónica, and González García Diego, Universidad de la República (Uruguay). Facultad de Psicología.
- Subjects
POLITICA SOCIAL ,POLITICA GUBERNAMENTAL ,ADOLESCENCIA ,URUGUAY ,PSICOLOGIA SOCIAL - Abstract
El interés de la siguiente tesis es producir conocimiento sobre la temática de niños, niñas y adolescentes (NNA) en situación de calle en Uruguay. La delimitación de la problemática consiste en establecer cómo se produce la construcción de las nociones de NNA en situación de calle a partir del análisis de la racionalidad de las políticas públicas, específicamente aquellas que se encargan de atender a dicha población. Los objetivos específicos son indagar cómo se construyen las nociones de sujeto NNA en situación de calle a partir de las políticas sociales focalizadas e indagar sobre los procedimientos, las estrategias y las tácticas de gobierno dirigidas a NNA en situación de calle. A través de una metodología cualitativa se analizan, desde una perspectiva genealógica, documentos oficiales, documentos de difusión y entrevistas a informantes calificados. Las técnicas de análisis aplicadas al material empírico refieren al análisis de contenido temático. Los referentes teóricos que sustentan la investigación son los actuales “estudios de Gubernamentalidad”. La perspectiva de la gubernamentalidad permite analizar la trama desplegada por las Políticas Públicas, como aquellas acciones dirigidas a conducir la conducta de las poblaciones. Los dispositivos de calle se engendran a finales de los años 80, en Uruguay, como una alternativa al modelo tutelar y estableciendo una nueva tecnología de gobierno para la infancia, apuntada hacia tres niveles estratégicos de intervención: el sujeto NNA en situación de calle, la familia y la comunidad. Las formas de saber que sustentan las nociones de sujeto de atención se organizan en tres ciclos discursivos: discursos profesionales, discursos científico-académicos y discursos gubernamentales.La investigación reflexiona sobre la imposibilidad de los dispositivos en capturar la totalidad de las formas subjetivas, produciendo permanentemente fugas que los reformulan y los traducen en otra cosa.
- Published
- 2015
25. A calibrated database of Raman spectra for natural silicate glasses: implications for modelling melt physical properties.
- Author
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Giordano, Daniele, González‐García, Diego, Russell, James K., Raneri, Simona, Bersani, Danilo, Fornasini, Laura, Di Genova, Danilo, Ferrando, Simona, Kaliwoda, Melanie, Lottici, Pier Paolo, Smit, Matthijs, and Dingwell, Donald B.
- Subjects
- *
RAMAN spectroscopy , *OBSIDIAN , *GLASS transition temperature , *MOLTEN glass , *LIGHT sources - Abstract
The physical properties of silicate melts are of critical importance for understanding magmatic and volcanic processes on Earth and other planets. Most physical properties of melts are, ultimately, a consequence of the structural organization of the melt. Robust and fully generalizable strategies for the prediction of properties of naturally occurring melts as functions of composition, temperature, and pressure remain a challenging goal. Given the structural origin of macroscopic properties, Raman spectroscopy of glasses, which provides information on melt and glass structure, may provide a useful technique to understanding and quantify variations in macroscopic melt properties. Here, with the aim of providing a generalizable model for predicting the viscosity of silicate melts, we present the results of a Raman spectroscopy campaign performed on 30 anhydrous multicomponent silicate glasses resulting from quenching of remelted and homogenized volcanic rocks and synthetic equivalents. The sample suite comprises one of the largest databases of multicomponent melts for which (a) chemical compositions and (b) physical properties (i.e., viscosity, fragility, heat capacity, and glass transition temperature) are known. Raman spectra have been collected using green light sources at wavelengths of 532 nm. Spectra were collected on the same sample suite in four independent laboratories involving instruments from different manufacturers and, thus, using different spectrometers, detectors, and analytical conditions. Our results are also compared and integrated with published data on some of the same samples derived from two others setups using green light sources with 514.5 and 532 nm wavelegths. For the same sample, the Raman spectra acquired using different setups show different intensities and intensity ratios. However, a strategy based on the ratio between the low‐ and high‐wavenumber peaks (R) was developed to standardize the data to normalized Raman ratios (Rn) and thus to remove interlaboratory differences. Using these advances, we predict melt viscosity solely with the use of Raman spectral measurements of multicomponent silicate glasses, thus demonstrating the potential of the method in describing physical properties of silicate melts. [ABSTRACT FROM AUTHOR]
- Published
- 2020
- Full Text
- View/download PDF
26. Pérdida de la patria potestad, adopción y consecuencias de la misma
- Author
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Universidade da Coruña. Facultade de Dereito, González García, Diego, Universidade da Coruña. Facultade de Dereito, and González García, Diego
- Published
- 2017
27. Experimental determination of major element diffusivity in natural high-K calc-alkaline silicate melts
- Author
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González-García, Diego, Behrens, Harald, Petrelli, Maurizio, Vetere, Francesco, Zezza, Angela, Morgavi, Daniele, and Perugini, Diego
- Published
- 2016
- Full Text
- View/download PDF
28. Water-enhanced interdiffusion of major elements between natural shoshonite and high-K rhyolite melts
- Author
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González-García, Diego, primary, Behrens, Harald, additional, Petrelli, Maurizio, additional, Vetere, Francesco, additional, Morgavi, Daniele, additional, Zhang, Chao, additional, and Perugini, Diego, additional
- Published
- 2017
- Full Text
- View/download PDF
29. Exponential decay of concentration variance during magma mixing: Robustness of a volcanic chronometer and implications for the homogenization of chemical heterogeneities in magmatic systems
- Author
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Rossi, Stefano, primary, Petrelli, Maurizio, additional, Morgavi, Daniele, additional, González-García, Diego, additional, Fischer, Lennart A., additional, Vetere, Francesco, additional, and Perugini, Diego, additional
- Published
- 2017
- Full Text
- View/download PDF
30. Fiesta y Sociedad en la isla de La Palma (Siglos XVI-XIX)
- Author
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González García, Diego Andrés and Arbelo García, Adolfo
- Subjects
Historia - Abstract
Este proyecto trata sobre la evolución de algunas de las fiestas en La Palma, desde el siglo XVI hasta el siglo XIX, y también analiza los cambios en la sociedad, y la medida en la que éstos se reflejan en las fiestas populares. En consonancia, a través de la historia de la cultura, estudiamos a las celebraciones públicas y su imbricación con la política, la sociedad, la economía y las mentalidades. De este modo, aportamos conocimientos sobre algunas tradiciones que han desaparecido, y que podrían formar parte de nuestro patrimonio inmaterial. This project deals with the evolution of some festivities in La Palma from XVI Century to XIX Century. It is also analysed in this project the changes in society, and to the extent that those changes are reflected in the popular party´s. Besides, throught the history of culture we study public celebrations and their independence with politics, society, economy and mentalities. In this way, we provide knowledge about some traditions that have vanished and could become part of our immaterial heritage.
- Published
- 2015
31. Definir para gobernar: políticas dirigidas a niños, niñas y adolescentes en situación de calle en Uruguay.
- Author
-
FAGUNDEZ-D'ANELLO, DANIEL and GONZÁLEZ-GARCÍA, DIEGO
- Published
- 2018
- Full Text
- View/download PDF
32. Geoquímica de las ortoanfibolitas y rocas metabásicas de Zarza la Mayor-Ceclavín (Cáceres, España)
- Author
-
González García, Diego, Rubio Ordóñez, Álvaro, Cuesta, Andrés, and Corretgé Castañón, Luis Guillermo
- Subjects
Geochemistry ,Extremadura ,Zarza la Mayor ,Geoquímica ,Metabasite ,Metabasita ,Ortoanfibolita ,Orthoamphibolite - Abstract
El stock granodiorítico-tonalítico de Zarza la Mayor (noroeste de Cáceres, España) está bordeado por afloramientos pequeños y discontinuos de rocas metabásicas de afinidades gabroicas a dioríticas, con texturas entre grano fino-medio y porfídicas. El presente estudio geoquímico muestra que estas rocas son composicionalmente equivalentes a basaltos subalcalinos de características toleíticas, mientras que los diagramas de discriminación tectonomagmática las sitúan en un contexto tectónico intraplaca, The granodioritic-tonalitic stock of Zarza la Mayor (western central Spain) is bordered by small, discontinuous outcrops of low grade metabasic rocks with gabbroic to dioritic affinities, ranging from fine-medium grained to porphyritic in texture. The present geochemical study demonstrates that these rocks are equivalent in composition to subalcalic tholeiitic basalt while tectono-magmatic discrimination diagrams place them in a within-plate tectonic environment
- Published
- 2011
33. Termobarometría y metamorfismo de las ortoanfibolitas de Zarza la Mayor-Ceclavín (Cáceres, España)
- Author
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González García, Diego, Rubio Ordóñez, Álvaro, Cuesta Fernández, Andrés, and Corretgé Castañón, Luis Guillermo
- Subjects
Metamorfismo ,Ortoanfibolita ,Geotermometría ,Geobarometría ,Metabasitas ,Cáceres - Abstract
Las ortoanfibolitas de Zarza la Mayor-Ceclavín (Cáceres, España) se encuentran bordeando el stock granodioritico-tonalítico de Zarza la Mayor a modo de orla discontinua. Son rocas de afinidad gabroica a gabrodioiritica que han sufrido una importante anfibolitización. El estudio mediante geotermometría y geobarometría indica presiones y temperaturas de 2,9-4,3 kbar y 632-750 ºC para el par anfíbol-plagioclasa, y 299-313 ºC para la clorita. Se sugiere una evolución metamórfico-metasomática en dos etapas, una primera magmática-tardimagmática o metamórfica de contacto de alta temperatura, que produce anfíbol a partir de la paragénesis primaria, y una segunda etapa de menor temperatura con formación de clorita y clinozoisita.
- Published
- 2011
34. Petrología y geoquímica de las rocas metabásicas de Zarza la Mayor-Ceclavín (Cáceres)
- Author
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González García, Diego and Corretgé Castañón, Luis Guillermo
- Subjects
ortoanfibolitas ,Petrología ,Geoquímica ,Cáceres - Abstract
El stock de Zarza la Mayor se sitúa en el nororeste de la provincia de Cáceres (España), entre las localidades de Zarza la Mayor y Ceclavín. Es un cuerpo granodiorítico-tonalítico de edad Ordovícica encajado en materiales del complejo esquisto-grauváquico (Vendiense-Cámbrico inferior). En torno al cuerpo intrusivo, y a modo de orla discontinua, se encuentran una serie de afloramientos de pequeñas dimensiones de rocas metabásicas (metagabros y algunas metadioritas). Los más próximos al plutón están intensamente anfibolitizados y los situados al norte son leucogabros con alteración hidrotermal. Las venas hidrotermales son comunes, y entre ellas destacan un reducido número de venas holoplagioclasicas. El presente trabajo está enfocado en el estudio de la petrología, geoquímica mineral y geoquímica de roca total de las rocas metabásicas y las venas plagioclásicas, con el objetivo de caracterizarlos petrológica y geoquímicamente y determinar sus posibles afinidades y relaciones con otras rocas similares del Macizo Ibérico.
- Published
- 2011
35. Geochemistry of the orthoamphibolites and metabasic rocks from Zarza la Mayor-Ceclavín (Cáceres, Spain)
- Author
-
González García, Diego, Rubio Ordóñez, Álvaro, Cuesta, Andrés, and Corretgé Castañón, Luis Guillermo
- Subjects
Geochemistry ,Extremadura ,Zarza la Mayor ,Geoquímica ,Metabasite ,Metabasita ,Ortoanfibolita ,Orthoamphibolite - Abstract
El stock granodiorítico-tonalítico de Zarza la Mayor (noroeste de Cáceres, España) está bordeado por afloramientos pequeños y discontinuos de rocas metabásicas de afinidades gabroicas a dioríticas, con texturas entre grano fino-medio y porfídicas. El presente estudio geoquímico muestra que estas rocas son composicionalmente equivalentes a basaltos subalcalinos de características toleíticas, mientras que los diagramas de discriminación tectonomagmática las sitúan en un contexto tectónico intraplaca The granodioritic-tonalitic stock of Zarza la Mayor (western central Spain) is bordered by small, discontinuous outcrops of low grade metabasic rocks with gabbroic to dioritic affinities, ranging from fine-medium grained to porphyritic in texture. The present geochemical study demonstrates that these rocks are equivalent in composition to subalcalic tholeiitic basalt while tectono-magmatic discrimination diagrams place them in a within-plate tectonic environment
- Published
- 2011
36. Raman Spectroscopy from Laboratory and Proximal to Remote Sensing: A Tool for the Volcanological Sciences
- Author
-
Giordano, Daniele, Russell, James K., González-García, Diego, Bersani, Danilo, Dingwell, Donald B., and Del Negro, Ciro
- Subjects
13. Climate action - Abstract
Here we explore and review some of the latest ideas and applications of Raman spectroscopy to the volcanological sciences. Firstly, we provide a brief overview of how Raman spectral analysis works and how spectra from silicate glasses are interpreted. We then look at specific applications of Raman spectral analysis to the volcanological sciences based on measurements on and studies of natural materials in the laboratory. We conclude by examining the potential for Raman spectral analysis to be used as a field based aid to volcano monitoring via in situ studies of proximal deposits and; perhaps; in remote sensing campaigns
37. Diseño de parámetros para la implementación de un centro de entrenamiento para recubrimientos electrostáticos en polvo
- Author
-
Gallardo Navarro, Laura Cristina and González García, Diego
- Subjects
Plan de negocios ,Capacitación de empleados ,Ingeniería Industrial ,Investigación de mercados - Abstract
Las ideas de nuevos negocios surgen como respuesta a necesidades de un mercado definido y de la consideración de las organizaciones emprendedoras que están en constante búsqueda de competitividad y mejoramiento, La investigación que se presentara a continuación será una guía útil para las organizaciones interesadas en un centro de formación para el trabajo con enfoque industrial en recubrimientos, el documento detalla el estudio de la necesidad de mercado y el plan de negocios para llevarlo a cabo. En el primer capítulo está integrado por el proceso de diseño para dicha investigación, describe el problema y pretende dar avance en el desarrollo de los objetivos, por otra parte incluye los marcos de referencia con la teoría necesaria para la elaboración de un plan de negocios y todo lo concerniente a la leyes que rigen el sistema educativo por los establecimiento públicos o privados que ofrecen servicios de educación y formación para el trabajo, además de las fuentes y técnicas que se van a utilizar para la recolección de la información. Los capítulos siguientes integran lo que tiene que ver con el desarrollo de la investigación. En primer lugar el lector encontrara el estudio de mercado donde se describe el servicio que se desea prestar junto con el análisis de la demanda y de la oferta existente proyectada, la demanda potencial insatisfecha y el análisis de viabilidad del proyecto. Posteriormente se encuentra el estudio técnico que integra los procesos productivos a desarrollar para la prestación del servicio educativo y la determinación del tamaño, localización y la ingeniería del proyecto. En el capítulo once se presenta la propuesta con el estudio financiero que contiene el análisis de los requerimientos y recursos e inversiones para desarrollar el proyecto, junto con las fuentes financiamiento y las respectivas proyecciones financieras. Finalmente, en el capítulo doce se encuentran las conclusiones del proyecto, allí se evalúan desde los ámbitos económico y social los futuros beneficios de los socios estratégicos, la comunidad y en consecuencia la viabilidad del proyecto Pregrado Ingeniero(a) Industrial
- Published
- 2014
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