Geomorphic expression of rapid Holocene silicic magma reservoir growth beneath Laguna del Maule, Chile.

The article focuses on gradual accumulation of rhyolitic magma in the upper crust beneath Laguna del Maule, Chile. It states that the rate of growth of a rhyolite-producing magma reservoir is determined through the measurement of a deformed paleoshore surface, isotopic dating of volcanism and surface exposure. It refers to the consistency of the long-term rate of magma input with reservoir freezing and pluton formation.