Proyectos

[vc_section el_class="container mx-auto align-items-center circle--pattern" css=".vc_custom_1648956589196{padding-top: 3rem !important;}"][vc_row el_class="pb-5"][vc_column][vc_wp_custommenu nav_menu="6"][uoh_breadcrumb_component automatic_breadcrumb="true"][uoh_title_component title_dropdown="big" title_decorator="true"]{{title}}[/uoh_title_component][vc_column_text css=""]This project aims to investigate how structural modifications of a dicationic derivative of azobenzene can affect the drug release and load capacity of its photoactive molecular aggregate. To evaluate this, three types of structural modifications are proposed. First, the introduction of functional groups on the photoactive nucleus of dicationic azobenzene is expected to shift the absorption band of the molecular photoswitch. Second, the replacement of the fluorescent organic cations over the structure of the molecular photoswitch, which confer luminescent and amphipathic properties to the system. And third, the modification of the length of the chains over the molecular photoswitch could change the aggregate size. To determine whether these potential modifications can modulate the light-induced release activity of the photoswitchable aggregate, an enzyme inhibitor will be loaded and released by illumination in the presence of the enzyme. Under this scenario, any modification of the enzymatic activity will be correlated with the drug's photorelease.[/vc_column_text][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649209804184{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5"][vc_row el_class="container mx-auto align-items-center p-md-0 pt-5"][vc_column el_class="p-0"][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649210787516{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5 pb-md-5"][vc_row el_class="container mx-auto align-items-center"][vc_column][/vc_column][/vc_row][/vc_section]

[vc_section el_class="container mx-auto align-items-center circle--pattern" css=".vc_custom_1648956589196{padding-top: 3rem !important;}"][vc_row el_class="pb-5"][vc_column][vc_wp_custommenu nav_menu="6"][uoh_breadcrumb_component automatic_breadcrumb="true"][uoh_title_component title_dropdown="big" title_decorator="true"]{{title}}[/uoh_title_component][vc_column_text css=""]Los tiempos actuales han facilitado nuevos medios de expresión e interacción como son las redes sociales. Estas plataformas, desde unos orígenes que bien podrían definirse como centrados en el entretenimiento, la comunicación interpersonal y la puesta en común de nuestra imagen e intereses, han pasado a convertirse en arenas de debates polarizados y nada edificantes. En este escenario, nos parece necesario preguntarnos: ¿cómo funciona la producción y circulación cross-plataforma de discursos de odio en las redes sociales chilenas en los últimos años? Para obtener una respuesta, confiamos en que una aproximación interdisciplinar emprendida por un equipo de comunicadores, lingüistas y cientistas de datos puede proporcionar una mirada más completa y compleja sobre este problema. Nuestro objetivo general es comprender el funcionamiento cross-plataforma de los discursos de odio producidos y puestos en circulación en las redes sociales en Chile a partir de las tendencias informativas más relevantes entre 2015 y 2023. Para ello requerimos: 1) caracterizar cuantitativa y cualitativamente los tipos de discursos de odio producidos y puestos en circulación en las redes sociales en Chile a partir de las tendencias informativas más relevantes entre 2015 y 2023; 2) identificar las cuentas de origen y diseminación que hacen posible tanto la producción como la circulación cross-plataforma de los tipos de discursos de odio y sus comentarios en las redes sociales en Chile, y; 3) analizar cualitativamente las estrategias lingüísticas y semióticas usadas sistemáticamente en la producción de los tipos de discursos de odio y sus comentarios. Además, y no menos importante, proponemos diseñar un kit de recursos digitales con ejemplos y recomendaciones para fomentar estrategias de formación ciudadana que ayuden a los/as usuarios/as de estas redes sociales a leer críticamente los discursos de odio y proyectar acciones para confrontarlos o neutralizarlos. Si bien esta es una acción de divulgación científica, nos parece necesario dar un pequeño paso que proyecte incluso futuras investigaciones aplicadas.[/vc_column_text][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649209804184{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5"][vc_row el_class="container mx-auto align-items-center p-md-0 pt-5"][vc_column el_class="p-0"][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649210787516{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5 pb-md-5"][vc_row el_class="container mx-auto align-items-center"][vc_column][/vc_column][/vc_row][/vc_section]

Overview: Mechanical wave propagation physics is related to traumatic brain injury mechanisms. For instance, nonlinear shear waves can form in the brain progressively with propagation, amplifying the acceleration locally. This phenomenon is compatible with axonal brain injury in which the lesions are localized far from the impact region. Within the brain, not only shear waves propagate. Especially when considering the brain is full of folds and surfaces, including the gray-white matter interface, which can be seen in Fig. 1. The abundance of interfaces or surfaces makes us hypothesize that surface waves might be crucial for describing the biomechanics of traumatic brain injury. The surface waves are named after the nature of the interface. A wave propagating in a solid-vacuum interface is known as a Rayleigh wave, a wave propagating in a solid-fluid interface is known as a Scholte wave, and a wave propagating in a solid-solid interface is known as a Stoneley wave. This last might propagate within an interface formed by two types of soft tissue. An example of this is the interfaces formed by the white and gray matter in the brain (see Fig. 1). Surface waves, although confined to a surface, can penetrate up to a wavelength. In the context of soft tissues, the typical frequencies of elastic waves that propagate are in the range of 10 to 300 Hz. At these frequencies, the wavelengths are on the order Figure 1: Section of a temporal of centimeters, creating the necessity of studying these waves at brain lobe. Image obtained from depth. Surface waves are not explored sufficiently in incompressible soft the visible human project [1]. solids yet. We recently measured Scholte waves at depth in these materials. However, we are not aware of measurements of Stoneley waves at depth in incompressible soft solids like brain matter or gelatin. The lack of this experimental evidence is due to the challenges of measuring deformation in opaque materials without disrupting the medium. Thus, the general objective of this proposal is to detect, describe and characterize the propagation of Stoneley waves in interfaces formed by two incompressible tissue-mimicking materials using Ultrafast Ultrasound elastography-related techniques. Methodology: Advanced ultrasound imaging techniques implemented on a highly customized ultrasound imaging platform designed for high frame-rate imaging will be used to characterize fundamental Stoneley wave physics propagating at the interfaces between two soft solids. We first will perform experiments in flats and simple interfaces to obtain the parameter space (shear modulus, density, and prestress) in which planar Stoneley waves exist. Then, we will explore the effects of the bonding condition between the two mediums on the dispersion relation. Third, we will investigate the interaction of the shape of the interface on the wave propagation, and lastly, we will intend to propagate Stonely waves into 3D inclusions. These observations will be achieved with a number of steps that integrate advancements in ultrasound imaging, algorithms that measure the deformation, and modeling. Custom two-dimensional and three-dimensional imaging sequences, designed for displacement tracking, will be implemented for a dedicated Linear and Matrix array transducer that has 128 or 1024 elements and can reach a spatial resolution of 200microns at a very high framerate in the order of 10000 frames per second (2D or 3D frames respectively). Expected results: The results of this proposal will elucidate the conditions that the two soft solids need to propagate Stoneley waves. These conditions refer to the combination of mechanical properties of the materials, such as shear modulus and density, and the prestress field needed. We expect to establish the effect that the bonding condition between the two soft solids has on the nature of the Stoneley wave. In particular, we will monitor how the Stoneley wave speed and dispersion change with different bonding conditions. We believe this phenomenology has implications in imaging technology, tumor diagnosis, and brain injury biomechanics.

[vc_section el_class="container mx-auto align-items-center circle--pattern" css=".vc_custom_1648956589196{padding-top: 3rem !important;}"][vc_row el_class="pb-5"][vc_column][vc_wp_custommenu nav_menu="6"][uoh_breadcrumb_component automatic_breadcrumb="true"][uoh_title_component title_dropdown="big" title_decorator="true"]{{title}}[/uoh_title_component][vc_column_text css=""]EPIGENOMIC PROGRAMMING IN THE EARLY FETAL BLOOD-BRAIN BARRIER BY GESTATIONAL HYPOXIA: CONSEQUENCES FOR THE NEURO-ENDOTHELIAL LIFESPAN.[/vc_column_text][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649209804184{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5"][vc_row el_class="container mx-auto align-items-center p-md-0 pt-5"][vc_column el_class="p-0"][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649210787516{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5 pb-md-5"][vc_row el_class="container mx-auto align-items-center"][vc_column][/vc_column][/vc_row][/vc_section]

[vc_section el_class="container mx-auto align-items-center circle--pattern" css=".vc_custom_1648956589196{padding-top: 3rem !important;}"][vc_row el_class="pb-5"][vc_column][vc_wp_custommenu nav_menu="6"][uoh_breadcrumb_component automatic_breadcrumb="true"][uoh_title_component title_dropdown="big" title_decorator="true"]{{title}}[/uoh_title_component][vc_column_text css=""]Se propone estudiar la miel orgánica monofloral de Quillay (Quillaja saponaria Molina), que es un árbol endémico de Chile central. La miel de Quillay es reconocida por sus características organolépticas y efectos biológicos, comparables a mieles como la miel de manuka. Esta miel junto con el quitosano y la gelatina se utilizarán para elaborar los hidrogeles. La CHH se esterilizará mediante radiación gamma para obtener miel de grado médico. A continuación, se estudiará la caracterización fisicoquímica de la CHH y su efecto in vitro e in vivo. La caracterización se llevará a cabo mediante la determinación de diferentes parámetros fisicoquímicos y por cromatografía líquida de ultra alto rendimiento-espectrometría de masas. También se determinará la capacidad antioxidante de la CHH. Tras esta caracterización química, se evaluará in vitro el perfil de eficacia y seguridad de la miel. Para ello, se medirá el efecto de la CHH sobre macrófagos, fibroblastos y S. pseudintermedius. Por último, se comprobará el efecto in vivo de esta formulación sobre la cicatrización de heridas en ratones. Para ello, se realizará un ensayo de cicatrización de heridas, junto con el análisis histopatológico de biopsias de heridas y la determinación de parámetros hematológicos, para evaluar los cambios locales y sistémicos en los animales objeto de estudio. Con este proyecto, esperamos verificar y obtener nueva información sobre la capacidad de cicatrización de la miel chilena aplicada en hidrogeles en heridas infectadas por S. pseudintermedius. Esto permitirá contar con más herramientas para tratar eficientemente este tipo de patologías en medicina veterinaria.[/vc_column_text][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649209804184{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5"][vc_row el_class="container mx-auto align-items-center p-md-0 pt-5"][vc_column el_class="p-0"][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649210787516{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5 pb-md-5"][vc_row el_class="container mx-auto align-items-center"][vc_column][/vc_column][/vc_row][/vc_section]

[vc_section el_class="container mx-auto align-items-center circle--pattern" css=".vc_custom_1648956589196{padding-top: 3rem !important;}"][vc_row el_class="pb-5"][vc_column][vc_wp_custommenu nav_menu="6"][uoh_breadcrumb_component automatic_breadcrumb="true"][uoh_title_component title_dropdown="big" title_decorator="true"]{{title}}[/uoh_title_component][vc_column_text css=""]Esta investigación se enmarca en discusiones del campo interdisciplinario de los estudios de desastre, contribuyendo a la comprensión del rol de las comunidades en la gobernanza del riesgo. Estando establecido que los desastres relacionados con amenazas naturales se explican por la vulnerabilidad social, diversas agendas de desarrollo promueven políticas que prevengan futuros eventos mediante la reducción de la vulnerabilidad o el aumento de la resiliencia. A pesar de esto, diversos grupos sociales no solo son mayormente afectados por desastres según su clase, género, etnia/raza, ubicación, etc., sino además son excluidos de las instancias formales de gestión del riesgo. Los desastres en definitiva son políticos y expresan dinámicas de desarrollo desigual. Como respuesta, habitantes de territorios en riesgo deben organizar iniciativas que permitan resistir y hacer frente a posibles desastres, incrementando su propia resiliencia. Al igual que los desastres y sus riesgos subyacentes, estas iniciativas se inscriben en el contexto social y político más amplio. Sin embargo, no sabemos cómo ciertas crisis y transformaciones sociales más amplias influyen en estas iniciativas de resiliencia. Esta investigación se centra en Chile y el fenómeno denominado estallido social. Aunque el proceso abierto por el estallido, con sus movilizaciones y discursos críticos, abría la posibilidad de un nuevo escenario político en el país, actualmente esto está en entredicho. A pesar de ello, es de suma relevancia analizar si este contexto influye en cómo se gobiernan los riesgos en territorios expuestos a amenazas naturales. Es decir, si del estallido social emergió un conjunto de demandas por mayor justicia social y ambiental, es fundamental entender si tales discursos y prácticas interactúan (o no) con iniciativas locales que potencien una resiliencia justa que promueva la igualdad y sustentabilidad territorial. Por ello, el objetivo general del proyecto es: Analizar cómo los habitantes de territorios en riesgo experimentaron el estallido social, y cómo esta experiencia influencia la organización y el funcionamiento de iniciativas colectivas de resiliencia justa.[/vc_column_text][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649209804184{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5"][vc_row el_class="container mx-auto align-items-center p-md-0 pt-5"][vc_column el_class="p-0"][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649210787516{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5 pb-md-5"][vc_row el_class="container mx-auto align-items-center"][vc_column][/vc_column][/vc_row][/vc_section]

[vc_section el_class="container mx-auto align-items-center circle--pattern" css=".vc_custom_1648956589196{padding-top: 3rem !important;}"][vc_row el_class="pb-5"][vc_column][vc_wp_custommenu nav_menu="6"][uoh_breadcrumb_component automatic_breadcrumb="true"][uoh_title_component title_dropdown="big" title_decorator="true"]{{title}}[/uoh_title_component][vc_column_text css=""]The brain is an energy intensive organ that requires a robust supply of nutrients and oxygen. The vasculature irrigating the brain is a huge and complex network of blood vessels fulfilling this requirement, while also protecting the neural tissue from blood-borne toxic substances. This regulated nutrient supply is accomplished by the formation of a highly selective molecular barrier, termed the blood-brain barrier (BBB). Dysfunction of the BBB or malformations of the vascular network are associated with pathological conditions that impair brain function, and can lead to death. Thus, appropriate morphogenesis and establishment of the brain vasculature is necessary for a healthy life. The brain vasculature forms during intrauterine development, matching brain growth in this same period. Anatomically, blood vessels grow first surrounding the brain primordium and then penetrate the parenchyma until they vascularize the periventricular zone. The molecular regulation of this patterned growth is not completely understood. Several signaling pathways are known to be involved in brain angiogenesis, including WNT, TGF-β, Hh, and NOTCH, which differentially regulate vascular growth. Recently, cholesterol has been shown to modulate angiogenic growth in other vascular beds by regulating the activity of the NOTCH pathway, suggesting that cholesterol levels could influence developmental angiogenesis in the brain. Interestingly, cholesterol is also required for signal transduction of the Hh pathway. In preliminary in vitro experiments, we have observed that brain endothelial cells activate an angiogenic program after cholesterol depletion. Here, we will extend those studies to in vivo models to determine the role of cholesterol in developmental brain angiogenesis. We propose that an increase in vascular cell cholesterol activates NOTCH and attenuates Hh signaling pathways, restricting sprouting angiogenesis and blood-brain barrier formation in mouse embryo brain vasculature. To test this hypothesis, we will study mouse embryos with altered cholesterol levels by dietary, pharmacological, and genetic manipulations. We expect these manipulations to induce a reduction or an increase in cholesterol levels in the brain vasculature during embryonic development, which we will evaluate by measuring cholesterol content in isolated vascular fragments. In all these models, we will (Specific aim 1) study vascularization in the brain during intrauterine development using immunofluorescence with specific antibodies against endothelium proteins. In addition, we will measure the levels of transcript and proteins of general key regulators of angiogenesis in isolated vascular fragments, using qPCR and Western blot. We will (Specific aim 2) also evaluate the state of the BBB in the brain vasculature of these models at a fetal stage when the barrier is already formed and functional. For this, we will use immunofluorescence to detect the presence of marker proteins of the BBB in vascular fragments, and we will measure their levels by Western blot. Further, we will test the functionality of the barrier by injecting a fluorescent tracer and evaluating its extravasation in the brain. Finally, we will (Specific aim 3) determine the activation of the NOTCH and Hh pathways in the brain vasculature of the models at the stage of maximal angiogenesis. We will use qPCR and Western blot to measure the levels of marker genes and proteins for these two pathways in vascular fragments, and Proximity Ligation In Situ Hybridization in tissue sections to evaluate the transcript levels of those markers in situ. We expect that the different models of dietary, pharmacological, and genetic interventions will increase or reduce cholesterol levels in the brain vasculature. These changes are expected to correlate with opposing effects on angiogenesis in the brain during development (i.e. low cholesterol will increase angiogenesis, while high cholesterol will inhibit it). In the same way, we expect that distinct cholesterol levels will have opposing effects on the integrity of the BBB. These changes in angiogenesis and BBB function are expected to be associated with concomitant disruption of the NOTCH and Hh pathways. In summary, in this proposal we aim to cover a knowledge gap regarding the role of cholesterol in the regulation of developmental angiogenesis in the brain. These experiments may uncover new mechanisms driving vascular growth and barrier establishment in the brain, which could lead to new strategies for the prevention and treatment of pathologies involving the brain vasculature.[/vc_column_text][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649209804184{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5"][vc_row el_class="container mx-auto align-items-center p-md-0 pt-5"][vc_column el_class="p-0"][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649210787516{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5 pb-md-5"][vc_row el_class="container mx-auto align-items-center"][vc_column][/vc_column][/vc_row][/vc_section]

[vc_section el_class="container mx-auto align-items-center circle--pattern" css=".vc_custom_1648956589196{padding-top: 3rem !important;}"][vc_row el_class="pb-5"][vc_column][vc_wp_custommenu nav_menu="6"][uoh_breadcrumb_component automatic_breadcrumb="true"][uoh_title_component title_dropdown="big" title_decorator="true"]{{title}}[/uoh_title_component][vc_column_text css=""]The project covers the following topics: vibrations, multiphase flow, and pipes. All of them are strongly related to Mechanical Engineering and its applications.[/vc_column_text][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649209804184{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5"][vc_row el_class="container mx-auto align-items-center p-md-0 pt-5"][vc_column el_class="p-0"][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649210787516{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5 pb-md-5"][vc_row el_class="container mx-auto align-items-center"][vc_column][/vc_column][/vc_row][/vc_section]

[vc_section el_class="container mx-auto align-items-center circle--pattern" css=".vc_custom_1648956589196{padding-top: 3rem !important;}"][vc_row el_class="pb-5"][vc_column][vc_wp_custommenu nav_menu="6"][uoh_breadcrumb_component automatic_breadcrumb="true"][uoh_title_component title_dropdown="big" title_decorator="true"]{{title}}[/uoh_title_component][vc_column_text css=""]Ocean Island Volcanoes (OIVs) and seamounts are one of the most common, prominent and rapidly formed but least studied (from a geological/volcanological point of view) features on Earth. OIVs, which represent only the summit section of a much larger volcanic edifice rising up from the sea floor, are highly vulnerable to geological hazards such as volcanism, seismic activity, mass wasting (caldera formation), landslides and rockfalls, and tsunamis. Specifically, a volcanic eruption on an OIV can mainly have a substantial impact on the local population, infrastructure and economy. It is then essential understand the characteristic behaviour and the ages of the recent eruptions of the volcano to enhance the capacity to identify future geological hazard processes such as eruptions, tsunamis, etc. In other words, to forecast how a volcano will behave, it is essential to identify, map and analyse the deposits from past eruptions and determine the ages of those deposits. However, this becomes more challenging on Ocean Island Volcanoes that have not experienced recent eruptions, such as Easter Island (Chile), but which may still pose a significant risk of future eruption. This proposal focuses on Easter Island (Rapa Nui or Isla de Pascua), an isolated southeast Pacific island with 7.750 inhabitants, that receives more than 100.000 tourists per year. This island has been catalogued as one of the 92 active volcanos of Chile by the Chilean mining and geological service, occupying the 46th position in its Volcanic Risk ranking. It was included taking into account the recent activity focused on Terevaka volcano and its peripheral vents and other factors as the population and infrastructures exposure and its high amount of visitors per year. Nevertheless, there is still a lack of robust geochronology and volcano-stratigraphy and morphometry for Easter Island, especially for these most recent eruptions. Therefore, a comprehensive study of its Holocene eruptions regarding their styles, a more accurate age determination, and a well identification of submarine volcanic centres around the island is still pending to evaluate its potential volcanic hazard. The main aim of this project is to identify and study the most recent eruptions of Easter Island, both onshore and offshore. This will allow understanding how and when they took place in terms of volume, diverse morphometric parameters, styles and their ages which will verify if the island is still active. To identify and characterize the style of the most recent eruptions (Holocene- last 11.700 Kyr) on the island it is planned to conduct geomorphologic and morhometryc analyses of subaerial and submarine recent volcanic deposits with and integrated onshore/offshore approach. Also, volcano-stratigraphy for the most recent cones and associated deposits onshore, with special attention to those hydrovolcanic eruptions will be analysed. To determine the number of Holocene eruptions on the island, 14C (for charcoal), 40Ar/39Ar (for rocks) techniques will be used. Moreover, we will identify and date tephras of lacustrine sedimentary records of the Rano Raraku, Rano Kao lakes and the Rano Aroi peat bog related to recent eruptions. A likely future eruption on the island or near its coasts would have negative and serious consequences; therefore, it is essential to undertake this scientific research aimed at improving the knowledge of the processes and their potential impacts. Furthermore, this study will also contribute to understanding the overall evolution of an interoceanic volcanic island whose results can be compared with other more studied OIVs in the world. In addition, this project will support undergraduate and graduate students, for whom this study will comprise most of their dissertation research, being an extraordinary opportunity for them. Moreover, this study will foster ongoing international collaboration, providing a pipeline for future student and faculty exchange, and will promote outreach educational experiences for the community, as well as more specialized seminars.[/vc_column_text][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649209804184{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5"][vc_row el_class="container mx-auto align-items-center p-md-0 pt-5"][vc_column el_class="p-0"][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649210787516{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5 pb-md-5"][vc_row el_class="container mx-auto align-items-center"][vc_column][/vc_column][/vc_row][/vc_section]

[vc_section el_class="container mx-auto align-items-center circle--pattern" css=".vc_custom_1648956589196{padding-top: 3rem !important;}"][vc_row el_class="pb-5"][vc_column][vc_wp_custommenu nav_menu="6"][uoh_breadcrumb_component automatic_breadcrumb="true"][uoh_title_component title_dropdown="big" title_decorator="true"]{{title}}[/uoh_title_component][vc_column_text css=""]The world's transition to using cleaner energy sources to address climate change has led to a sharp rise in the demand for base and precious metals. Consequently, discovering new ore deposits to meet this growing demand and prevent supply shortages has emerged as one of the greatest challenges of the 21st century. Discovery of new magmatic-hydrothermal ore deposits can be improved based on a fundamental understanding of the geological processes that control the flux and focusing of ore-constituting elements in the Earth’s crust, and by identifying the differences between the bulk-rock and mineral chemistry of ore-forming and ordinary—barren—granitoids. Large metal anomalies in the Earth’s upper crust, such as porphyry copper-(molybdenum) deposits (PCDs), occur in intimate association with oxidized and water-rich arc magmatism in subduction zones. However, these deposits occur in restricted crustal domains and form in response to specific tectono-magmatic events, indicating that not all arc magmas have the same ore-forming potential. Understanding why only some magmas produced large PCDs while most other arc magmas remain barren is a fundamental scientific question and key to developing efficient exploration strategies. The volatile element composition of arc magmas, including water, sulfur, and halogens such as chlorine and fluorine, as well as their oxygen fugacity, exert a critical control on their ore-forming potential (i.e., ore fertility). These components are not only key to the complexation and transport of ore metals during hydrothermal activity, but also influence the amount of ore metals transported by magmas and the efficiency to which they are transferred from magmas to exsolved fluids. Magmatic differentiation in lower crustal hot zones beneath thick crustal regions is expected to enhance the volatile element budget and oxygen fugacity of evolving magmas that are discharged to the upper crust. This occurs due to the accumulation of incompatible volatile elements during successive cycles of recharge by mafic magmas and crystallization, facilitated by the deeper and hotter conditions beneath thicker arc crusts. As such, an increasingly recognized hypothesis holds that ore-forming magmas display a particularly increased budget of volatile elements and higher oxygen fugacities when compared to barren arc magmas, and that this is largely influenced by the arc crust thickness. The proposed work will test this hypothesis by focusing on the Miocene to Mio-Pliocene magmatism and associated world-class PCD mineralization in the Andes of central Chile. From the Early Miocene to the Mio-Pliocene, the arc segment located between latitudes ~33–34.5° S in the Andes of central Chile has seen a continued increase in crustal thickness and has evolved from being barren in the Early Miocene to producing some of the largest PCDs of the world in the Mio-Pliocene, such as El Teniente and Rio Blanco-Los Bronces. This geological scenario and the spatial and age distribution of the associated outcropping intrusive rocks offer a unique opportunity to investigate the temporal evolution of the volatile composition of magmas and its consequences for ore fertility. The goal of this proposal is to examine, adopting a regional scale perspective, the evolution in the volatile composition and oxygen fugacity of magmas produced in this arc segment and its relationship to magmatic ore fertility, as well as how this may have been influenced by changes in crustal thickness. To achieve this, I will sample an extensive suite of granitoids that represent a continuum from Early Miocene to Mio-Pliocene magmas, including porphyry-forming intrusions. By combining zircon petrochronology, apatite, biotite, and amphibole mineral chemistry, in conjunction with the bulk-rock composition of intermediate to felsic intrusive rocks, I will be able to constrain relative changes in the hydration state, sulfur contents, halogen and oxygen fugacities, as well as in their associated crustal thickness during the evolution of the selected arc segment. This will be done by implementing a combination of cutting-edge analytical techniques, including synchrotron-based sulfur X-ray absorption near edge structure spectroscopy, electron probe microanalysis, (laser ablation) inductively coupled plasma mass spectrometry, and X-ray fluorescence spectrometry. I aim at (1) testing the differences in the volatile composition of barren and ore-forming intrusive rocks; (2) determining whether there is a gradual change in the volatile systematics of magmas during the evolution of the studied arc segment; and (3) analyzing the relationship between variations in crustal thickness and the volatile composition of associated magmas. The results of this proposal will lead to a better understanding of the magmatic controls underpinning the formation of giant PCDs and will provide valuable insights into identifying the differences between the bulk-rock and mineral chemistry of ore-forming and barren granitoids as tools for vectoring mineralized regions.[/vc_column_text][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649209804184{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5"][vc_row el_class="container mx-auto align-items-center p-md-0 pt-5"][vc_column el_class="p-0"][/vc_column][/vc_row][/vc_section][vc_section css=".vc_custom_1649210787516{background-color: #f6faff !important;}" el_class="p-md-0 pt-md-5 pb-md-5"][vc_row el_class="container mx-auto align-items-center"][vc_column][/vc_column][/vc_row][/vc_section]