Abstract
Side-scan sonar images from the Lower Valencia Fan show that turbidite bedforms (chevrons) and net sediment aggradation vary around a small fault scarp. One or more turbidity currents were affected by the fault, but the exact timing of the fault movement in relation to the chevrons is not known. A scaled laboratory experiment showed that mean flow vector would not be affected by a current flowing over an obstacle of similar height to flow depth ratio.
Original language | English |
---|---|
Pages (from-to) | 165-171 |
Number of pages | 7 |
Journal | Geo-Marine Letters |
Volume | 18 |
Issue number | 2 |
DOIs | |
Publication status | Published - Dec 1998 |