H metasomatism
Xem 1-1 trên 1 kết quả H metasomatism
-
The Yenipazar deposit of volcanogenic sulfide occurrence, situated approximately 9 km SW of Yenipazar, is hosted in quartzmuscovite schists and gneiss. Following the Late Cretaceous, the quartz-mica schists and gneiss have been altered to clay minerals, resulting in important kaolin deposits.
21p viminotaur2711 30-10-2019 13 1 Download
CHỦ ĐỀ BẠN MUỐN TÌM
TOP DOWNLOAD