Tectonic controls on the transition from homogeneous crystal-rich to zoned crystal-poor ignimbrites

Lu TY, He ZY, Bachmann O, Klemd R, Yan LL, Xu XS (2026)


Publication Type: Journal article

Publication year: 2026

Journal

Book Volume: 7

Article Number: 539

Journal Issue: 1

DOI: 10.1038/s43247-026-03523-x

Abstract

Silicic calderas exhibit cyclic magmatic progression, with some systems transitioning from homogeneous crystal-rich to subsequent zoned crystal-poor caldera-forming eruptions—yet mechanisms governing this shift remain elusive. Here we contrast two caldera-forming eruptions from the Furongshan caldera complex in Southeast China. Our integrated zircon oxygen-hafnium isotopes, trace elements and bulk-rock data revealing a distinct shift from homogeneous crystal-rich tuffs to compositionally zoned crystal-poor tuffs, accompanied by a decrease in water content and oxygen fugacity. We attribute this temporal shift to a tectonic transition from water-fluxed melting linked to slab dehydration, a hallmark of classical arc magmatism, to adiabatic decompression melting driven by asthenospheric upwelling associated with the progressively rollback subduction of the paleo-Pacific plate. Our findings reveal that large magmatic systems record plate-scale tectonic reorganization via marked shifts in magma water contents and the petrological traits of volcanic deposits.

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APA:

Lu, T.Y., He, Z.Y., Bachmann, O., Klemd, R., Yan, L.L., & Xu, X.S. (2026). Tectonic controls on the transition from homogeneous crystal-rich to zoned crystal-poor ignimbrites. Communications Earth & Environment, 7(1). https://doi.org/10.1038/s43247-026-03523-x

MLA:

Lu, Tian Yu, et al. "Tectonic controls on the transition from homogeneous crystal-rich to zoned crystal-poor ignimbrites." Communications Earth & Environment 7.1 (2026).

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