A5034702880- Geological and Geochemical Analysis
- Geochemistry and Geologic Mapping
- Geological and Tectonic Studies in Latin America
- Geological and Geophysical Studies Worldwide
- earthquake and tectonic studies
- Geothermal Energy Systems and Applications
- High-pressure geophysics and materials
- Geophysical and Geoelectrical Methods
- Environmental and Ecological Studies
- Geology and Paleoclimatology Research
- Environmental and Cultural Studies in Latin America and Beyond
- Geological and Geophysical Studies
- Geophysical Methods and Applications
- Accounting and Financial Management
- CO2 Sequestration and Geologic Interactions
- Hydrocarbon exploration and reservoir analysis
National University of Salta
2016-2022
Consejo Nacional de Investigaciones Científicas y Técnicas
2016-2022
Centro Científico Tecnológico - San Juan
2022
Instituto de Química del Noroeste Argentino
2020
Subduction zones represent the interface between Earth’s interior (crust and mantle) exterior (atmosphere oceans), where carbon other volatile elements are actively cycled Earth reservoirs by plate tectonics. Helium is a sensitive tracer of sources can be used to deconvolute mantle crustal in arcs; however it not thought recycled into subduction processes. In contrast, readily recycled, mostly form carbon-rich sediments, thus understand delivery via subduction. Further, chemically-reactive...
This study presents new stratigraphic, structural and hydrogeological data on the Tocomar geothermal volcanic area (Puna plateau, Central Andes, NW Argentina), together with preliminary geochemical magnetotelluric data. The main reservoir is located within fractured Pre-Palaeozoic–Ordovician units. recharged by meteoric waters. Geothermal fluids upwell where regional structures intersect secondary associated development of basin. Preliminary indicate a temperature ∼ 200° C local gradient...
This paper presents a detailed geological map at the 1:20,000 scale of Tocomar basin in Central Puna (north-western Argentina), which extends over an area about 80 km2 and displays spatial distribution Quaternary deposits structures that cover Ordovician basement Tertiary sedimentary volcanic units. The new dataset includes litho-facies descriptions, stratigraphic structural data 234U/230Th ages for travertine rocks. reconstructed framework, along with analysis, has revealed complex...
One of the most outstanding features Southern Puna is occurrence a widespread monogenetic mafic volcanism during Neogene-Quaternary. Despite number published papers focusing on petrogenesis this back-arc volcanism, works aimed its physical volcanology are scarce. This paper presents characterization in Pasto Ventura region, located southeast edge Puna. The results show that region there low density small-volume eruptive centers aligned with regional tectonic structures and significant...
Arc magmatism plays a key-role in the growth and differentiation of continental crust. In particular, prolonged magmatic flux events control genesis deep crustal hot zones where magma accumulation fractionation favour arc crust evolution geochemical stratification. this view long-lived systems located domains, with their erupted products spanning from basalts to rhyolites are formidable archive for understanding transcrustal plumbing construction stratified This study focuses on (ca. 9 Ma)...