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Magma titanium and iron contents dictate crystallization timescales and rheological behaviour in basaltic volcanic systems - Communications Earth & Environment

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Magma titanium and iron contents dictate crystallization timescales and rheological behaviour in basaltic volcanic systems - Communications Earth & Environment

Magma ascending through Earth's crust undergoes complex chemical and physical changes that may induce crystallization, a process that contributes to lead the magmatic system toward a thermodynamic state of equilibrium. The diverse cooling and deformative regimes suffered by magmas heavily influence crystallization rates, solidification timescales, and consequently, the rheological evolution of magma.

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Magma titanium and iron contents dictate crystallization timescales and rheological behaviour in basaltic volcanic systems - Communications Earth & Environment

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Magma titanium and iron contents dictate crystallization timescales and rheological behaviour in basaltic volcanic systems - Communications Earth & Environment

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