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 |
|---|---|
| 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
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Rikhvanov, L. P., Sarnayev, S. I., & Bezkhodarnova, T. E. (1985). Skarn radiogeochemical features. Geochemistry International, 22(6), 144-157.