Uncovers the dynamics of gas channels in silicic magmas, indicating formation factors and implications for volcanic activity.
• The development of gas channels in immobile magmas depends on multiple factors. • Bubble coalescence is a dynamic process controlled by gas and crystal content. • The evolution of channelling can be tracked by observing bubble textures. • Phenocrysts facilitate permeable chains formation but ultimately cause their rupture.
No takes yet. Share an insight, caveat, or question.
Theurel et al. (2026) studied this question.
Synapse has enriched 5 closely related papers on similar clinical questions. Consider them for comparative context: