Article ID Journal Published Year Pages File Type
4716539 Lithos 2012 17 Pages PDF
Abstract
► The albitized rock in Forsmark originated close to the peak regional metamorphism. ► Basic magmatism during the regional metamorphism has triggered the albitization. ► The episyenite formation in Forsmark occurred between or after 1.8-1.7 Ga. ► Geometry and distribution of the episyenites argue against high fluid/rock ratios. ► The influence of the altered rocks is negligible for a geological repository.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
Authors
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