Towards scientific forecasting of magmatic eruptions
Forecasting eruptions is a fundamental goal of volcanology. However, difficulties in
identifying eruptive precursors, fragmented approaches and lack of resources make eruption …
identifying eruptive precursors, fragmented approaches and lack of resources make eruption …
Evolution of the East African Rift System from trap-scale to plate-scale rifting
Many continental rifts are subjected to volcanism in tandem with rifting, which has raised a
long-standing debate about whether magmatism is the cause or the consequence of plate …
long-standing debate about whether magmatism is the cause or the consequence of plate …
Structure of volcano plumbing systems: A review of multi-parametric effects
A Tibaldi - Journal of Volcanology and Geothermal Research, 2015 - Elsevier
Magma is transported and stored in the crust mostly through networks of planar structures
(intrusive sheets), ranging from vertical dykes to inclined sheets and horizontal sills, and …
(intrusive sheets), ranging from vertical dykes to inclined sheets and horizontal sills, and …
Oblique rift opening revealed by reoccurring magma injection in central Iceland
Extension deficit builds up over centuries at divergent plate boundaries and is recurrently
removed during rifting events, accompanied by magma intrusions and transient metre-scale …
removed during rifting events, accompanied by magma intrusions and transient metre-scale …
Magnetotelluric image of transcrustal magmatic system beneath the Tulu Moye geothermal prospect in the Ethiopian Rift
F Samrock, AV Grayver, H Eysteinsson… - Geophysical Research …, 2018 - Wiley Online Library
Continental rifting is initiated by a dynamic interplay between tectonic stretching and mantle
upwelling. Decompression melting assists continental breakup through lithospheric …
upwelling. Decompression melting assists continental breakup through lithospheric …
[HTML][HTML] The eruptive history and magmatic evolution of Aluto volcano: new insights into silicic peralkaline volcanism in the Ethiopian rift
The silicic peralkaline volcanoes of the East African Rift are some of the least studied
volcanoes on Earth. Here we bring together new constraints from fieldwork, remote sensing …
volcanoes on Earth. Here we bring together new constraints from fieldwork, remote sensing …
Large-to local-scale control of pre-existing structures on continental rifting: Examples from the Main Ethiopian Rift, East Africa
In the Main Ethiopian Rift (East Africa) a complex tectonic history preceded Tertiary rifting
creating pre-existing discontinuities that influenced extension-related deformation …
creating pre-existing discontinuities that influenced extension-related deformation …
A review of laboratory and numerical modelling in volcanology
JL Kavanagh, SL Engwell, SA Martin - Solid Earth, 2018 - se.copernicus.org
Modelling has been used in the study of volcanic systems for more than 100 years, building
upon the approach first applied by Sir James Hall in 1815. Informed by observations of …
upon the approach first applied by Sir James Hall in 1815. Informed by observations of …
How caldera collapse shapes the shallow emplacement and transfer of magma in active volcanoes
Calderas are topographic depressions formed by the collapse of a partly drained magma
reservoir. At volcanic edifices with calderas, eruptive fissures can circumscribe the outer …
reservoir. At volcanic edifices with calderas, eruptive fissures can circumscribe the outer …
The origin of along‐rift variations in faulting and magmatism in the Ethiopian Rift
The geological record at rifts and margins worldwide often reveals considerable along‐strike
variations in volumes of extruded and intruded igneous rocks. These variations may be the …
variations in volumes of extruded and intruded igneous rocks. These variations may be the …