THE GEOLOGY AND STRUCTURE OF NEOGENE ROCKS IN DADYAL AND ADJACENT AREAS, IN THE SUB-HIMALAYAS, AZAD JAMMU AND KASHMIR, PAKISTAN
Journal Title: Earth Sciences Malaysia - Year 2017, Vol 1, Issue 1
Abstract
The project area lies along the western limb of the Hazara Kashmir Syntaxis. The Hazara Kashmir Syntaxis is an antiformal structure. The project area includes Dadyal, Bihari, Ratta, Sammorthala, Samlotha, Dhingar, Panwar and Karara Saiyidan. The Late Miocene to Recent Himalayan Neogene rocks are exposed in the core of the syntaxis. These Neogene rocks include the Kamlial Formation, Chinji Formation, Nagri Formation, Dhok Pathan Formation, Soan Formation and Recent alluvium. The major folds in the project area include the Mirpur syncline, Pheran Dinpur anticline and Sadaqabad Syncline. The folds are northwest-southeast trending and southwest or northeast vergent, asymmetric and open. The only fault in the project area is Ratta Fault. The Ratta Fault is a reverse fault. The northwest southeast trending folds and faults are the result of northeast southwest Himalayan compression in the area.
Authors and Affiliations
Ahmer Bilal, Muhammad Yasin, Ahtasham Ali
Keywords
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- EP ID EP261867
- DOI 10.26480/esmy.01.2017.15.20
- Views 63
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