A refined genetic model for the Laisvall and Vassbo
Three stages of porosity fill were recognized: (1) P-REE-bearing minerals such as anatase, hydrothermal monazite, and fluorapatite; (2) calcite, barite, quartz, K-feldspar, and fluorite cements; and (3) sulfides (galena, sphalerite, and pyrite; Figs. 4, 5, 6, and 7). At the two deposits, a "pre-Pb-Zn sulfide stage" and a "Pb-Zn sulfide ...