Abstract
The clay mineralogy of Cromer Forest-bed Formation sediments at West Runton, Norfolk is characterised by; 1) low kaolinite abundance, typically
| Original language | English |
|---|---|
| Pages (from-to) | 63-78 |
| Number of pages | 16 |
| Journal | Bulletin of the Geological Society of Norfolk |
| Issue number | 58 |
| Publication status | Published - 2008 |