From Magma Formation to Eruption: Temperature Path of Two Late Carboniferous Post‐Collisional Calderas (Bohemian Massif)

Abstract The thermal evolution of magmatic systems of the Altenberg‐Teplice and Tharandter Wald calderas, which erupted during the terminal post‐collisional phase of the Variscan orogeny in the Bohemian Massif, was investigated. The zircon saturation temperatures and Ti‐in‐zircon thermometer indicat...

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Hlavní autoři:	I. Olšanská, F. Tomek, C. Robustelli Test, E. Zanella, M. Svojtka, J. Trubač, F. Cifelli, F. Finger
Médium:	Artigo
Jazyk:	Inglês
Vydáno:	Wiley 2025-05-01
Edice:	Geochemistry, Geophysics, Geosystems
Témata:	collapse caldera magma emplacement magnetic susceptibility thermoremanent magnetization Ti‐in‐zircon thermometry Bohemian Massif
On-line přístup:	https://doi.org/10.1029/2025GC012217
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