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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Үндсэн зохиолчид:	I. Olšanská, F. Tomek, C. Robustelli Test, E. Zanella, M. Svojtka, J. Trubač, F. Cifelli, F. Finger
Формат:	Artigo
Хэл сонгох:	Inglês
Хэвлэсэн:	Wiley 2025-05-01
Цуврал:	Geochemistry, Geophysics, Geosystems
Нөхцлүүд:	collapse caldera magma emplacement magnetic susceptibility thermoremanent magnetization Ti‐in‐zircon thermometry Bohemian Massif
Онлайн хандалт:	https://doi.org/10.1029/2025GC012217
Шошгууд:	Шошго нэмэх Шошго байхгүй, Энэхүү баримтыг шошголох эхний хүн болох!