Ti3+ in corundum traces crystal growth in a highly reduced magma

Aggregates of corundum crystals with skeletal to hopper morphology occur in pyroclastic rocks erupted from Cretaceous basaltic volcanoes on Mt Carmel, N. Israel. The rapid growth of the crystals trapped volumes of the parental Al2O3-supersaturated melt; phenocrysts of tistarite (Ti2O3) in the trapped melts indicate crystallization at oxygen fugacities 6-7 log units below the Iron-Wustite buffer (fO(2)= Delta IW - 6 to - 7), induced by fluxes of mantle-derived CH4-H-2 fluids. Cathodoluminescence images reveal growth zoning within the individual crystals of the aggregates, related to the substitution of Ti3+ in the corundum structure. Ti contents are<0.3 wt% initially, then increase first linearly, then exponentially, toward adjacent melt pockets to reach values>2 wt%. Numerical modelling indicates that the first skeletal crystals grew in an open system, from a moving magma. The subsequent linear increase in Ti reflects growth in a partially closed system, with decreasing porosity; the exponential increase in Ti close to melt pockets reflects closed-system growth, leading to dramatic increases in incompatible-element concentrations in the residual melts. We suggest that the corundum aggregates grew in melt/fluid conduits; diffusion modelling implies timescales of days to years before crystallization was terminated by explosive eruption. These processes probably operate in explosive volcanic systems in several tectonic settings.

Automated summary

The study reveals aggregates of corundum crystals with skeletal to hopper morphology in pyroclastic rocks erupted from Cretaceous basaltic volcanoes on Mt Carmel, N. Israel. The growth of these crystals trapped volumes of the parental melt and phenocrysts of tistarite in the trapped melts suggest crystallization at specific oxygen fugacities. Cathodoluminescence images show growth zoning within individual crystals, linked to the substitution of Ti3+ in the corundum structure.