Volatile resorption expedites eruption onset in large silicic systems. [PDF]
Keller F, Townsend M, Troch J, Huber C.
europepmc +1 more source
Reconstructing magmatic histories with 3D diffusion modeling of complex crystals. [PDF]
Mourey AJ, Mutch EJF.
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Fissure locations and fire-fountain dynamics during the December 2023-September 2024 Svartsengi Volcanic System eruptions, Iceland, from aerial imagery and recreational webcam footage. [PDF]
Rhodes RS +4 more
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Shared genetic architecture between Crohn's disease and IgA nephropathy: implications for a gut-immune-kidney axis. [PDF]
Su T +12 more
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Large-scale pleiotropic analysis across cancers reveals shared genetic mechanisms and identifies novel functional genes. [PDF]
Wu X +7 more
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Magma supply, magma ascent and the style of volcanic eruptions
Earth and Planetary Science Letters, 2007Abstract We propose a new way of looking at the sequence of events leading to different styles of silicic, volcanic eruptions. Small-to-medium sized eruptions, either explosive or effusive, are explained by the ascent of isolated magma batches from mid-crustal magma chambers.
Katharine Cashman, Roberto Scandone
exaly +3 more sources
Properties of the Magma and Modified Magma Equations
Journal of the Physical Society of Japan, 1990Solutions of the “magma equation”, f t =[ f n {( f - m f t ) x -1}] x , are investigated for compact support initial conditions. It is shown analytically that traveling wave solutions with compact support do not exist for this equation. Numerical integration demonstrates that although initial conditions with compact support produce solitary waves ...
Daisuke Takahashi +2 more
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Silicic Magmas (Magma Formation in the Crust)
1971In deeply eroded ancient fold regions, levels are exposed at which silicic magma was once generated. From the field of abyssal geology proper, we now move over to conditions of investigation more customary to us, and it may be comparatively easy to draw some conclusions.
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The redox state is one of the master variables behind the Earth's forming processes, which at depth concern magma as the major transport agent. Understanding redox exchanges in magmas is pivotal for reconstructing the history and compositional make-up of our planet, for exploring its mineral resources, and for monitoring and forecasting volcanic ...
Moretti R., Neuville D. R.
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The dynamics of magma mixing in a rising magma batch
Bulletin Of Volcanology, 1989The conditions under which two magmas can become mixed within a rising magma batch are investigated by scaling analyses and fluid-dynamical experiments. The results of scaling analyses show that the fluid behaviours in a squeezed conduit are determined mainly by the dimensionless number
Takehiro Koyaguchi, Stephen Blake
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