Geological and environmental controls on the change of eruptive style (phreatomagmatic to Strombolian-effusive) of Late Pleistocene El Caracol tuff cone and its comparison with adjacent volcanoes around the Zacapu basin (Michoacán, México)
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文摘

We identify a tuff cone complex amid of a scoria cone dominated MGVF.

We study its morphology, tectonic configuration and sedimentological characteristics of the deposits.

The system fails to achieve optimal water–magma ratio due to high magma flux and hardly-sufficient water supply conditions.

The eruption style changes from Surtseyan/weak phreatomagmatic to fully magmatic (Strombolian to effusive).

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