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Zircon geochronology suggests a long-living and active magmatic system beneath the Ciomadul volcanic dome field (eastern...

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

Magma diversity reflects recharge regime and thermal structure of the crust

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

Magmatic pulse driven by sea-level changes associated with the Messinian salinity crisis

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

Machine Learning Thermo‐Barometry: Application to Clinopyroxene‐Bearing Magmas

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

A Recurrent Magmatic Pattern on Observable Timescales Prior to Plinian Eruptions From Nevado de Toluca (Mexico)

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

Stochastic modelling of deep magmatic controls on porphyry copper deposit endowment

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

A Data Driven Approach to Investigate the Chemical Variability of Clinopyroxenes From the 2014–2015 Holuhraun–Bárda...

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

Estimates of Volume and Magma Input in Crustal Magmatic Systems from Zircon Geochronology: The Effect of Modeling Assump...

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

The role of H2O on the extraction of melt from crystallising magmas

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

Tectonic controls on global variations of large-magnitude explosive eruptions in volcanic arcs

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

Classification, segmentation and correlation of zoned minerals

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

Quantitative chemical mapping of plagioclase as a tool for the interpretation of volcanic stratigraphy: an example from ...

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

Does the Shape of a Volcano Reflect Its Personality?

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

A cross correlation method for chemical profiles in minerals, with an application to zircons of the Kilgore Tuff (USA)

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

Evidence for Residual Melt Extraction in the Takidani Pluton, Central Japan

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

Tempo of magma degassing and the genesis of porphyry copper deposits

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

Magmatic evolution of zoned and unzoned ignimbrites: evidence for a complex crustal architecture feeding four rapid-sequ...

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

Modulation of magmatic processes by CO 2 flushing

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

Determining the current size and state of subvolcanic magma reservoirs

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

Regional variability in the frequency and magnitude of large explosive volcanic eruptions

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

Caldera resurgence driven by magma viscosity contrasts

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

Magma Degassing as a Source of Long‐Term Seismicity at Volcanoes: The Ischia Island (Italy) Case

Project: FEVER

Updated at: 27-04-2024

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The Long-Term Life-Cycle of Nevado de Toluca Volcano (Mexico): Insights Into the Origin of Petrologic Modes

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

The build-up and triggers of volcanic eruptions

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

Investigating Complex Isochron Data Using Mixture Models

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

Periodic Reporting for period 4 - FEVER (Forecasting the recurrence rate of volcanic eruptions)

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

CO 2 favours the accumulation of excess fluids in felsic magmas

Project: FEVER

Updated at: 27-04-2024

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Project acronym FEVER

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Zircon geochronology suggests a long-living and active magmatic system beneath the Ciomadul volcanic dome field (eastern...

Magma diversity reflects recharge regime and thermal structure of the crust

Magmatic pulse driven by sea-level changes associated with the Messinian salinity crisis

Machine Learning Thermo‐Barometry: Application to Clinopyroxene‐Bearing Magmas

A Recurrent Magmatic Pattern on Observable Timescales Prior to Plinian Eruptions From Nevado de Toluca (Mexico)

Stochastic modelling of deep magmatic controls on porphyry copper deposit endowment

A Data Driven Approach to Investigate the Chemical Variability of Clinopyroxenes From the 2014–2015 Holuhraun–Bárda...

Estimates of Volume and Magma Input in Crustal Magmatic Systems from Zircon Geochronology: The Effect of Modeling Assump...

The role of H2O on the extraction of melt from crystallising magmas

Tectonic controls on global variations of large-magnitude explosive eruptions in volcanic arcs

Classification, segmentation and correlation of zoned minerals

Quantitative chemical mapping of plagioclase as a tool for the interpretation of volcanic stratigraphy: an example from ...

Does the Shape of a Volcano Reflect Its Personality?

A cross correlation method for chemical profiles in minerals, with an application to zircons of the Kilgore Tuff (USA)

Evidence for Residual Melt Extraction in the Takidani Pluton, Central Japan

Tempo of magma degassing and the genesis of porphyry copper deposits

Magmatic evolution of zoned and unzoned ignimbrites: evidence for a complex crustal architecture feeding four rapid-sequ...

Modulation of magmatic processes by CO 2 flushing

Determining the current size and state of subvolcanic magma reservoirs

Regional variability in the frequency and magnitude of large explosive volcanic eruptions

Caldera resurgence driven by magma viscosity contrasts

Magma Degassing as a Source of Long‐Term Seismicity at Volcanoes: The Ischia Island (Italy) Case

The Long-Term Life-Cycle of Nevado de Toluca Volcano (Mexico): Insights Into the Origin of Petrologic Modes

The build-up and triggers of volcanic eruptions

Investigating Complex Isochron Data Using Mixture Models

Periodic Reporting for period 4 - FEVER (Forecasting the recurrence rate of volcanic eruptions)

CO 2 favours the accumulation of excess fluids in felsic magmas