%0 Journal Article
%@ 00167622
%A Iqbal, O.
%A Baig, M.S.
%A Pervez, S.
%A Siddiqi, M.I.
%D 2018
%F scholars:10915
%I Geological Society of India
%J Journal of the Geological Society of India
%K crustal structure; faulting; fold and thrust belt; GIS; Miocene; stratigraphy; thrust fault, India; Jammu and Kashmir; Pakistan
%N 1
%P 57-66
%R 10.1007/s12594-018-0820-2
%T Structure and stratigraphy of Rumbli and Panjar areas of Kashmir and Pakistan with the aid of GIS
%U https://khub.utp.edu.my/scholars/10915/
%V 91
%X The project area lies in the southern part of the Hazara Kashmir syntaxis. The Hazara Kashmir syntaxis is an antiformal structure. The project area includes Rumbli, Namb, Chatrora, Chachan, Panjar, Barathian and Utrinna areas of Rawalpindi and Sudhnoti districts. The southeastern limb of the Hazara Kashmir syntaxis is imbricated along Punjal thrust, Main Boundary thrust and Riasi fault. The Jhelum fault truncates the western limb of Hazara Kashmir syntaxis. The core of syntaxis comprises of Himalayan molasse deposits. These molasse deposits represent the part of cover sequence of Indian plate. These Himalayan molasse deposits include the Early to Middle Miocene Kamlial Formation, Middle to Late Miocene Chinji Formation, Late Miocene Nagri Formation and Late Miocene Dhok Pathan Formation. The area is highly deformed resulting folds and faults. The major folds in the project area are the Panjar anticline, Barathian syncline, Barathian anticline, Rumbli anticline, Chatrora antiformal syncline and Namb syncline. The folds are either northwest-southeast trending or southwestnortheast trending. The folds are asymmetric, open, and gentle and close in nature. The folds are southwest, northeast or southeast vergent. The Jhelum fault truncates the northeast and northwest trending structures. The folds and faults are the result of northeastsouthwest or northwest-southeast Himalayan compression. © 2018, Geological Society of India.
%Z cited By 3