There is a picture snapped near Margalla region, Pakistan. Here recumbent fold and an associated fault forming a structure having close affinity with the drag type folding.
Photo credit: Rana Asif, Director Geoscience, Advance Research Laboratory, Islamabad, Pakistan (December, 2013).
A collection of outcrop photos having traced fold and fault features from quaternary deposits (neotectonic features) is presented with due permission from Rayees Ahmad Shah.
Outcrop of the Northern Suture Zone (Main Karakorum Thrust) on Taghafiri Ridge, extending north from Rakaposhi Mountain and above the town of Minapin, Gilgit-Baltistan: personal photo (looking northwest), 1986; google earth (looking west), 2016. The shear zone here consists of multiple ultrabasic phyllitic mylonite units. The bright yellowish white rock is boudinaged actinolite schist. There is also talc-dolomite schist and chlorite schist with cubic pyrite. The ridge rises to Rakaposhi peak (to the south and left) which is ophiolitic. The Northern Suture Zone lies within the upper stratigraphic section of the ophiolitic sequence, which is overturned and youngs downsection and to the north (dipping steeply south).