Greenschists from Kranjska Reber
AbstractThe low grade metamorphic rocks of Kranjska Reber Mt. have been derived from volcanic rocks of spilite-keratophyre association and some sedimentary rocks. The metamorphism took place under the P, T environment corresponding to the very beginning of the greenschist facies, that is to the quartz-albite-muscovite-chlorite subfacies. Critical minerals occurring in different associations are stilpnomelane and tremolite. They indicate Alpine metamorphism, if the rock sequence as supposed by geologists is of Middle Triassic age.
How to Cite
Hinterlechner-Ravnik, A. (1978). Greenschists from Kranjska Reber. Geologija, 21(2), 245–253. Retrieved from https://www.geologija-revija.si/index.php/geologija/article/view/442