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Gianluca Norini

Researcher at National Autonomous University of Mexico

Publications -  75
Citations -  1617

Gianluca Norini is an academic researcher from National Autonomous University of Mexico. The author has contributed to research in topics: Volcano & Geothermal gradient. The author has an hindex of 23, co-authored 70 publications receiving 1304 citations. Previous affiliations of Gianluca Norini include University of Milan & National Institute of Geophysics and Volcanology.

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Reconstruction of the eruptive activity on the NE sector of Stromboli volcano: timing of flank eruptions since 15 ka

TL;DR: In this paper, a multidisciplinary geological and compositional investigation allowed the authors to reconstruct the occurrence of flank eruptions on the lower NE flank of Stromboli volcano since 15 ka.
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Pulsating flow dynamics of sustained, forced pyroclastic density currents: insights from a facies analysis of the Campo de la Piedra Pómez ignimbrite, southern Puna, Argentina

TL;DR: The Quaternary Campo de la Piedra Pomez ignimbrite (CPPI) as discussed by the authors was formed by sustained PDCs, generated from a low fountain eruptive style (boiling over), with overall flow conditions characterized by high particle concentration and limited capability to surmount topographic obstacles.
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Geochemical mapping, environmental assessment and Pb isotopic signatures of geogenic and anthropogenic sources in three localities in SW Spain with different land use and geology

TL;DR: In this paper, the concentration of harmful chemical elements in the soil of three case study areas in the Huelva Province are analyzed and related with the land use and local geology, showing that anomalies of harmful elements are present in the topsoil of the three areas, even in the rural Aroche site, where neither industrial nor mining activities occur.
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The geological and structural evolution of the long-lived Miocene-Pleistocene La Hoyada Volcanic Complex in the geodynamic framework of the Central Andes, Argentina

TL;DR: In this article, a new stratigraphic framework for the eastern Cordillera de San Buenaventura, composed by four supersynthems separated by unconformities that reflect periods of quiescence of the volcanic activity, catastrophic destructive events and changes in the magmatic plumbing system, is proposed.