Sedimentiogical study for subsurface section of Abu Khasib
Keywords:
Abu Khasib, Sediment, Fossils, Dolomite, Baghdad
Abstract
Abu Khasib formation, east of Baghdad, is studied via checking (95) thin section collected from a field east of Baghdad, in terms of fossils and minerals. The limestone of the studied area consists of skeletal grains like planktonic foraminifera, echinoderms and algae, and these stones have micrite groundmass, whereas,Peloids is an example for non-skeletal grains. The most prominent digenetic processes are cementation, delomitization and dissolution