The Structure Geology of District Kotli in the Sub Himalayas: A Case Study in Pakistan
سال انتشار: 1399
نوع سند: مقاله کنفرانسی
زبان: انگلیسی
مشاهده: 172
فایل این مقاله در 10 صفحه با فرمت PDF قابل دریافت می باشد
- صدور گواهی نمایه سازی
- من نویسنده این مقاله هستم
استخراج به نرم افزارهای پژوهشی:
شناسه ملی سند علمی:
GSI39_111
تاریخ نمایه سازی: 22 اردیبهشت 1400
چکیده مقاله:
In the present work, we deal with the structure geology, structural maps, stereo plotting and preparation of structural cross-sections of Tatta Pani, Dandli, Sarsawa and Phagwari areas of the Kotli district along the eastern limb of the Hazara-Kashmir syntaxis. This is an active fold-and-thrust belt in the sub Himalayas of Pakistan. The Mandi syncline, Tatta Pani Anticline, Panjera anticline and Khuirata anticline are the major folds. These are open in nature. The Riasi Thrust, Godri Badshah and Nuoi Sarhota Fault are the major Faults. The Riasi Thrust and Godri Badshah Fault are active faults. The Cambrian to Recent sedimentary rock sequence is exposed in the area. The area lies between the latitude ۳۳°۳۱ ۴۴"to ۳۳°۳۳۲۲" and longitude ۷۳°۴۵۰" to ۷۳°۵۹۰" on Survey of Pakistan Toposheet number ۴۳G/۱۴. The ۷۲ Km۲ area has been mapped on scale of ۱:۵۰,۰۰۰
کلیدواژه ها:
نویسندگان
Enayatollah Emami Meybodi
Assistant Prof, Department of Geology Yazd University Yazd, Iran
Syed Khaliq Hussain
Department of Geology Yazd University Yazd, Iran
Sayed Muhammad Hanif
Institute of Geology University of Azad Jammu and Kashmir Muzaffarabad, Pakistan.