Abstract
The elevated uranium levels in Devonian acid volcanites are syngenetic. The contrasty volcanic series has a single common Rb-Sr isochron corresponding to 413±13 My and indicates a single magmatic source for the acid and basic effusives. The original Sr ratio in the magma source was 0.7043±0.0006 and corresponds to the range of similar values for island-arc basalts (0.7033-0.7051). It is assumed that the generation of the magmas involved mantle material. -Journal summary
| Original language | English |
|---|---|
| Pages (from-to) | 69-79 |
| Number of pages | 11 |
| Journal | Geochemistry International |
| Volume | 25 |
| Issue number | 7 |
| Publication status | Published - 1988 |
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ASJC Scopus subject areas
- Geochemistry and Petrology
- Geophysics
Cite this
Rikhvanov, L. P., Plyusnin, G. S., Yershov, V. V., Komarnitskiy, G. M., Pakhol'chenko, Y. A., & Sandimirova, G. P. (1988). The origin of south Siberian radiogeochemically specialized volcanites. Geochemistry International, 25(7), 69-79.