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- W3233614 abstract "Petrographic investigation of the Grand-Halleux boreholes identified different generations of quartz veins that were formed during different periods of fluid migration in an environment that was decreasingly influenced by compressive deformation. The Ar-40-Ar-39 dating of muscovite associated with shear zones crosscutting two quartz vein generations indicated an age of 318 +/- 4.7Ma, which allows determining the position of the different vein generations in relation to the Variscan deformation in the Stavelot-Venn Massif. This age also determines the approximate age for the Variscan syn-orogenic metamorphism in the Stavelot-Venn Massif. Younger extension veins and prismatic quartz crystals in open spaces are associated with different generations of carbonates, associated with Pb-Zn-Cu mineralisation. This implies that this mineralisation did not form during Caledonian metamorphism or early Variscan orogenic metamorphism, but has a late to post-Variscan age. It could be linked to the post-orogenic expulsion of metamorphic fluids, but a link with the younger Pb-Zn mineralisation in the Variscan front zone is favoured based on the presence of high-salinity low temperature fluids." @default.
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- W3233614 date "2014-01-01" @default.
- W3233614 modified "2023-09-24" @default.
- W3233614 title "Timing of veining and Variscan deformation in the Stavelot-Venn Massif (Belgium)" @default.
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