Massimo D'Antonio

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Full Professor

Università degli Studi di Napoli Federico II

Italy

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Recent Grants

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Timing of Magmatic Processes at Campi Flegrei volcanic complex

Open Date: 2015-05-01

Close Date: 2016-05-01

Grant: Close

Ricerca Dipartimentale

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PRIN-COFIN

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Articles (10)

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2022

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2022

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2022

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2022

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2021

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2021

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2021

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2021

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2021

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2021

Collaborators (4)

Carlo Pelullo

Istituto Nazionale di Geofisica e Vulcanologia

ITALY

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Sandro Conticelli

Professor

Università degli Studi di Napoli Federico II

ITALY

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Raffaella Silvia Iovine

Istituto Nazionale di Geofisica e Vulcanologia

ITALY

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Alessandro Fabbrizio

University of Milano-Bicocca

ITALY

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Massimo D'Antonio

Research Interests

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Recent Grants

Articles (10)

Linking the Mediterranean MIS 5 tephra markers to Campi Flegrei (southern Italy) 109–92 ka explosive activity and refining the chronology of MIS 5c-d millennial-scale climate variability

Petrogenesis of Miocene igneous rocks in the Tafresh area (central Urumieh‐Dokhtar magmatic arc, Iran): Insights into mantle sources and geodynamic processes

Sr-Nd Isotopic Composition of Pyroxenes as a Provenance Indicator of a Double-Volcanic Source in Sands of the Ofanto River (Southern Italy)

Mineral-Melt Equilibria and Geothermobarometry of Campi Flegrei Magmas: Inferences for Magma Storage Conditions

A Messinian Gypsum Deposit in the Ionian Forearc Basin (Benestare, Calabria, Southern Italy): Origin and Paleoenvironmental Indications

Petrography and Mineral Chemistry of Monte Epomeo Green Tuff, Ischia Island, South Italy: Constraints for Identification of the Y-7 Tephrostratigraphic Marker in Distal Sequences of the Central Mediterranean

Constraints from geochemistry, zircon U-Pb geochronology and Hf-Nd isotopic compositions on the origin of Cenozoic volcanic rocks from central Urumieh-Dokhtar magmatic arc, Iran

Hydrothermal alteration in Eshtehard volcanoes, Iran: Constraints from trace elements redistribution and stable isotope geochemistry

Mediterranean tephrostratigraphy and peri-Tyrrhenian explosive activity revaluated in light of the 430-365 ka record from Fucino Basin (central Italy)

Olivine melilitites, mantle xenoliths, and xenocrysts of the Takarindiona district: Petrogenesis, magmatic evolution, and the sub-continental lithospheric mantle of east-central Madagascar

Collaborators (4)

Carlo Pelullo

Sandro Conticelli

Raffaella Silvia Iovine

Alessandro Fabbrizio

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