Lots of anticlines with apparent Quaternary activity. Folds are asymmetric, north vergent. A few possible fault scarps, but most scarps appear to be related to fold limbs. Definitely active folds, however. Individual folds are on the order of 50 km long, in fold trends that are up to 200 km long.
Folds are en echelon in each trend suggesting lateral component.
One fold appears to be deforming the modern mud flats along the coast east of Kandla. No idea yet. Many rivers and washes draining the folds have impressive flights of fluvial terraces, suggesting fairly rapid uplift of folds. Great future Ph. Everything is okay.