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Analyzes magmatic processes in various tectonic settings, suggesting new insights into volcanic behavior.
C/s, as determined by diffusive water loss and Mg diffusion, respectively. Our approach offers a transferable framework to constrain the timescales of volatile degassing and magmatic processes across diverse tectonic settings on Earth and beyond, thereby enhancing our understanding of magma evolution, eruption dynamics, and volcanic hazards.
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Mourey et al. (2026) studied this question.
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