Abstract
Plio/Quaternary fluvial sandstones and conglomerates within the Sorbas Basin, SE Spain contain a number of well preserved deformation features ranging from relatively small scale faulting, to soft sediment deformation structures (clastic dykes; soft sediment folding; soft sediment mixing bodies) and relatively larger scale syn-sedimentary folding. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 57-65 |
| Number of pages | 0 |
| Journal | Quaternary Proceedings |
| Volume | 3 |
| Issue number | 0 |
| Publication status | Published - 1 Jan 1993 |