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Multiphase solid inclusions in garnet pyroxenite – evidence of carbonate-silicate metasomatism in the mantle, Saxothuringian Zone, Bohemian Massif (2025/2)Hýbl, T., Kotková, J., Čopjaková, R., 2025: Multifázové pevné inkluze v granátickém pyroxenitu – doklad karbonáto-silikátové metasomatózy v plášti, saxothuringikum, Český masiv. – Acta Mus. Morav., Sci. Geol., 110, 2, 419–436 (with English summary)
Multiphase solid inclusions in garnet pyroxenite – evidence of carbonate-silicate metasomatism in the mantle, Saxothuringian Zone, Bohemian Massif
The studied pyroxenite forms ~1–2 cm thick veins cutting garnet peridotite in a quarry north of the village of Zoblitz.…
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Secondary bastnäsite-(Ce), bastnäsite-(La) and parisite-(Ce) from the Cínovec deposit – products of interaction of primary REE minerals with late low-temperature fluids (2023/1)Hreus, S., Cempírek, J., Breiter, K., Výravský, J., 2023: Sekundární bastnäsit-(Ce), bastnäsit-(La) a parisit-(Ce) z ložiska Cínovec – produkty interakce primárních REE minerálů s pozdními nízkoteplotními fluidy. – Acta Mus. Morav., Sci. Geol., 108, 1, 29–40 (with English summary)
Secondary bastnäsite-(Ce), bastnäsite-(La) and parisite-(Ce) from the Cínovec deposit – products of interaction of primary REE minerals with late low-temperature fluids
The Cínovec/Zinnwald is a world-class greisen-type Li-Sn-W-Nb-Ta deposit. The REE minerals as common accessories are…
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