Modification of pre-existing folds in a shear zone: A case study from Kumbhalgarh–Ranakpur area, South Delhi Fold Belt, Rajasthan, India

A review on deformation structures of different terranes in the Precambrian Aravalli-Delhi Mobile Belt (ADMB), NW India: Tectonic implications and global correlation

“…1b) and is marked by several large-scale NE-SW trending DF2 antiforms and synforms (Kamlighat and Goramghat areas, Gupta et al, 1997) with the PSZ and KSZ continuing further south. Within these shear zones, the fold axis of small-scale DF1 and DF2 folds are reoriented to the NW-SE direction parallel to the direction of slip due to inhomogeneous shear (Choudhury et al, 2016;Hatui and Chattopadhyay, 2020). E-W directed late-stage strike-slip faults cross-cut the entire width of SDT, at Todgarh, Deogarh, Chhapli, Gogunda, etc.…”

U–Pb geochronology and metamorphic history of gneissic rocks from Sarwar‐Junia Fault Zone, Rajasthan, NW India: Implications for the tectonothermal evolution of the Aravalli‐Delhi Mobile Belt

“…For example, the Rakhabdev shear zone (Sarkar et al, 2020) in the east and the Phulad shear zone in the west (Chatterjee et al, 2017, 2020) are two major terrain‐bounding lineaments. The deformation style and age of the Phulad shear zone are well studied (Chatterjee et al, 2017; Ghosh et al, 2003; Hatui & Chattopadhyay, 2020). However, the North‐South lineaments in the eastern side, and several less‐studied East‐West striking fault zones disposed at a high angle to these major lineaments, are not properly studied.…”