[PDF][PDF] Strzegom-Sobótka massif (Sudetes, SW Poland)–an example of a complex late-Variscan granitic intrusion and its pegmatitic mineralization
J Ciesielczuk, J Domańska-Siuda… - Mineralogia–Special …, 2008 - academia.edu
Mineralogia–Special Papers, 2008•academia.edu
Since the XIXth century the Strzegom-Sobótka granitic massif is regarded as one of the
classical occurrences of intragranitic miarolitic and vein pegmatites famous for their complex
hydrothermal mineral assemblages. The tour is intended to present the participants with the
recent state of knowledge on various aspects of magmatic and postmagmatic evolution of
these pegmatites and the host granites. Mineralogical clou of the trip are visits to working
quarries providing the unique opportunity of collecting fresh samples.
classical occurrences of intragranitic miarolitic and vein pegmatites famous for their complex
hydrothermal mineral assemblages. The tour is intended to present the participants with the
recent state of knowledge on various aspects of magmatic and postmagmatic evolution of
these pegmatites and the host granites. Mineralogical clou of the trip are visits to working
quarries providing the unique opportunity of collecting fresh samples.
Abstract
Since the XIXth century the Strzegom-Sobótka granitic massif is regarded as one of the classical occurrences of intragranitic miarolitic and vein pegmatites famous for their complex hydrothermal mineral assemblages. The tour is intended to present the participants with the recent state of knowledge on various aspects of magmatic and postmagmatic evolution of these pegmatites and the host granites. Mineralogical clou of the trip are visits to working quarries providing the unique opportunity of collecting fresh samples.
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