Dersleri yüzünden oldukça stresli bir ruh haline sikiş hikayeleri bürünüp özel matematik dersinden önce rahatlayabilmek için amatör pornolar kendisini yatak odasına kapatan genç adam telefonundan porno resimleri açtığı porno filmini keyifle seyir ederek yatağını mobil porno okşar ruh dinlendirici olduğunu iddia ettikleri özel sex resim bir masaj salonunda çalışan genç masör hem sağlık hem de huzur sikiş için gelip masaj yaptıracak olan kadını gördüğünde porn nutku tutulur tüm gün boyu seksi lezbiyenleri sikiş dikizleyerek onları en savunmasız anlarında fotoğraflayan azılı erkek lavaboya geçerek fotoğraflara bakıp koca yarağını keyifle okşamaya başlar
GET THE APP
Theory Of Continental Drift And Plate Tectonics | 12133
ISSN: 2157-7617
Journal of Earth Science & Climatic Change
Open Access
Our Group organises 3000+ Global Conferenceseries Events every year across USA, Europe & Asia with support from 1000 more scientific Societies and Publishes 700+ Open Access Journals which contains over 50000 eminent personalities, reputed scientists as editorial board members.
T
he study area includes Dheri Qasim, Bela Bhadarsha, Pipli, Nalamuslamanan, Doberan and Khad of Azad Kashmir and
Pakistan. The area lies along the western limb of the Hazara-Kashmir Syntaxis in the sub-Himalayas of Pakistan. The study
area is the part of Kashmir folds-and-thrust belt which is formed after the collision of the Indian and Eurasian plates.
The lithostratigraphic units exposed in the project area are the rocks of the Rawalpindi and Siwalik Groups. The Formations
exposed include the Early to Middle Miocene Kamlial Formation, Middle to Late Miocene Chinji Formation, Late Miocene
Nagri Formation, Late Miocene Dhok Pathan Formation, Pliocene Soan Formation, Pleistocene Mirpur Formation and Recent
Alluvium.
Structurally, the area is highly deformed. The folds and faults are present in the area. The Rajdahni syncline, Malair anticline,
Malair syncline, Chouk Bourjan syncline, Chouk Bourjan anticline, Panjar syncline and Panjar anticline are the major folds
developed in the area. The folds are isoclinal, tight, open and northwest to southeast vergent.
The major faults in the area are thrust; reverse and strike slip in nature. These faults include Chillayar Fault, Malikpur-Diljaba
Fault, Malair Fault and Jhelum Fault.
Biography
Waqas Mehmood has completed B.Sc. in Applied Geology & M.Sc. in Geology from University of Azad Jammu and Kashmir Muzaffarabad, Pakistan in 2012.
Relevant Topics
Peer Reviewed Journals
Make the best use of Scientific Research and information from our 700 + peer reviewed, Open Access Journals