マグマレオロジーの分子スケールでの理解：時分割放射光x線回折・散乱実験からのアプローチ

Abstract

Magma rheology is a key factor in understanding and modelling volcanic eruptions. Until now, macroscopic rheology experiments reveal the viscosity of the magma and conditions at which shear thinning and brittle failure occur. However, it remains unclear what mechanisms control complex magma rheology from the atomic and molecular-scale structure perspective. More specifically, no experimental data on A d v a n c e P u b l i c a t i o n