Abstract
Data are given on the behaviour of U and Th during skarn formation. The concentrations and forms of these elements in main skarn minerals are considered. The skarns in the region are characterized by an influx of U and reduction in the Th/U ratios. The elevated U concentrations were produced by infiltrating hydrothermal solutions.-C.N.
Original language | English |
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Pages (from-to) | 144-157 |
Number of pages | 14 |
Journal | Geochemistry International |
Volume | 22 |
Issue number | 6 |
Publication status | Published - 1985 |
ASJC Scopus subject areas
- Geochemistry and Petrology
- Geophysics