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Opalized Serpentinites in Central Serbia by Miodrag Filipović is a document available to read on EtoBox.
What is Opalized Serpentinites in Central Serbia about?
This document summarizes research on opalized serpentinite occurrences in central Serbia. The serpentinite originated from ultramafic rocks that were part of the Jurassic Tethyan ophiolite sequence. During the Tertiary, hydrothermal activity associated with magmatism opalized the serpentinite along fracture zones. Analysis showed the opal is predominantly tridymite-cristobalite type opal-CT. Opalized serpentinite deposits could be used industrially and indicate other potential hydrothermal mineralization in
- Author
- Miodrag Filipović
- Language
- EN