Abstract
Redox front processes in rocks are important in the context of both radioactive waste disposal and the development of orebodies. A study is reported of uranium and thorium distributions and natural decay series disequilibrium abut a redox front in a granite from southwest Scotland. The results are placed in the context of large-scale aqueous transport of uranium in the region and are compared with those obtained in a previous study of redox front processes in phonolitic rocks in Brazil. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 139-146 |
| Number of pages | 8 |
| Journal | Transactions - Institution of Mining & Metallurgy, Section B |
| Volume | 101 |
| Issue number | Sept-Dec |
| Publication status | Published - 1992 |