Magma Plumbing Systems
A special issue of Minerals (ISSN 2075-163X). This special issue belongs to the section "Mineral Deposits".
Deadline for manuscript submissions: closed (15 November 2020) | Viewed by 5196
Special Issue Editor
Special Issue Information
Dear Colleagues,
Our understanding of how melt is stored and feeds active volcanoes has dramatically changed in recent years. We have moved away from ideas of a simple “chamber” of magma sitting beneath a volcano to more complex networks of melt, mush and crystals that extend throughout the crust and into the uppermost mantle. This network plays an integral role in eruption dynamics where an influx of fresh, hot magmas from deep in the crust/mantle into a shallower reservoir accompanied by mixing, convective overturn and self-mixing may trigger volcanic eruptions. Timescales of such pre-eruptive magmatic processes are recorded by the chemically zoned minerals within volcanic rocks and can be unlocked by means of diffusion chronometry. In the last 20 years or so, our ability to geophysically and geodetically understand pre-eruptive magmatic processes has greatly improved. The use of seismic data to locate earthquakes has allowed us to image magma movement with unprecedented resolution. However, reconciling the dynamics of magmatic systems and processes (e.g., magma mobilisation and eruption) with volcano deformation and monitoring data is still an open challenge. The ultimate goal of this Special Issue it to put together scientific contributions investigating architectures and dynamics of magma plumbing systems from different perspectives including but not limited to petrology, volcanology, geophysics and geodetic. Interdisciplinary contributions are particularly encouraged.
Dr. Chiara Maria Petrone
Guest Editor
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Keywords
- Magmatic processes
- Crystal residence time
- Crystal cargo
- Magma remobilization and eruption
- Melt movement
- Magma mixing
- Volcano deformation
- Magma degassing.
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