Abstract
The occurrence of Middle Oligocene rocks in Ashdagh Mountain is previously studied like Baba and Bajwan Formations; both of them belong to Middle Oligocene age; the former Formation represents reef- forereef deposits, while the latter one represents reef- backreef deposits. But Tarjil Formation was not studied in the mountain which is complementary of both Baba and Bajwan Formations and represents forereef- open sea- offshore deposits of the same age. The aim of this study is proving the occurrence of Middle Oligocene sedimentary rock of Tarjil Formation.
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CITATION STYLE
Kharajiany, S. (2013). The Middle Oligocene Rock Strata (Tarjil Formation) in Ashdagh Mountain, Sangaw District, Sulaimani Governorate, Kurdistan Region , NE Iraq. Journal of Zankoy Sulaimani - Part A, 15(3), 119–132. https://doi.org/10.17656/jzs.10262
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