Alberto Caselli

ORCID: 0000-0002-0457-1607
Publications
Citations
Views
---
Saved
---
About
Contact & Profiles
Research Areas
  • Geology and Paleoclimatology Research
  • Geological and Geochemical Analysis
  • earthquake and tectonic studies
  • Geological and Tectonic Studies in Latin America
  • Geochemistry and Geologic Mapping
  • Geological formations and processes
  • Polar Research and Ecology
  • Geological and Geophysical Studies Worldwide
  • Cryospheric studies and observations
  • Environmental and Ecological Studies
  • Seismic Waves and Analysis
  • Seismology and Earthquake Studies
  • Paleontology and Stratigraphy of Fossils
  • Geomagnetism and Paleomagnetism Studies
  • Environmental and Cultural Studies in Latin America and Beyond
  • Groundwater and Isotope Geochemistry
  • Climate change and permafrost
  • High-pressure geophysics and materials
  • Landslides and related hazards
  • Geophysical and Geoelectrical Methods
  • Earthquake Detection and Analysis
  • Paleontology and Evolutionary Biology
  • Methane Hydrates and Related Phenomena
  • Pleistocene-Era Hominins and Archaeology
  • Archaeology and Cultural Heritage

National University of Río Negro
2014-2023

Consejo Nacional de Investigaciones Científicas y Técnicas
1998-2022

Centro Científico Tecnológico - San Juan
2016-2022

University of Buenos Aires
2002-2015

Fundación Ciencias Exactas y Naturales
2005-2015

Institute of Astronomy and Space Physics
2004-2012

Universidad San Pablo CEU
2004

Universidad San Pablo
2004

Universidad Bicentenaria de Aragua
2002

Abstract Here we report on the first assessment of volatile fluxes from hyperacid crater lake hosted within summit Copahue, a very active volcano Argentina‐Chile border. Our observations were performed using variety in situ and remote sensing techniques during field campaigns March 2013, when an fumarole field, 2014, acidic volcanic covered field. In latter campaign, found that 566 to 1373 t d −1 SO 2 being emitted plume appeared largely invisible. This, combined with our derived bulk...

10.1002/2015jb012160 article EN Journal of Geophysical Research Solid Earth 2015-08-13

Synthetic Aperture Radar (SAR) Differential Interferometry (DInSAR) and its extensions to manage time series are nowadays well-known mastered techniques perform among others land-motion monitoring. We present here a fully automated monitoring service based on DInSAR Multidimensional Small Baseline Subset (MSBAS) methods. The processing chain named "InSAR Mass Toolbox for multidimensional Time series" (MasTer) is demonstrated with the peculiar case of Laguna del Maule Domuyo volcanoes, which...

10.1016/j.jsames.2020.102850 article EN cc-by-nc-nd Journal of South American Earth Sciences 2020-09-02

Abstract The integration of inverse thermal history modeling new geochronological data with structural analyses from the western flank Domuyo volcano (∼36°30′S) allows us to propose a detailed cooling key region in Southern Andes. area is located northwestern part Chos Malal fold‐and‐thrust belt back‐arc Despite extensive geological investigations this region, details about early stages Andean deformation remain poorly understood. present study focuses on interpretation and U‐Pb, fission...

10.1029/2020tc006415 article EN Tectonics 2021-05-18

Abstract The crater lake and associated hydrothermal features of Copahue volcano have been studied intensively over the last 20 years (1995–2015). geochemical isotopic compositions waters provide insights into processes occurring in volcanic–hydrothermal system, thermal springs. Variations temperature chemical composition reveal fundamental changes system that precede accompany magmatic phreatic eruptive events at Copahue. A conceptual model summit was developed involving intrusion slivers...

10.1144/sp437.16 article EN Geological Society London Special Publications 2016-12-23

Planchón-Peteroa volcano started a renewed eruptive period between January 2010 and July 2011. This was characterized by the occurrence of 4 explosive phases, dominated low-intensity phreatic activity, which produced almost permanent gas/steam columns (200-800 m height over active crater). Those presented frequently scarce ash, were interrupted explosions that ash 1,000-3,000 in more intense periods. Eruptive plumes transported several directions (NW, N, NE, E SE), but than half time plume...

10.5027/andgeov43n1-a02 article EN cc-by Andean geology 2015-09-30
Coming Soon ...