Lithostratigraphy & microfacies analysis of Avanah Formation (Middle Eocene) in Gomaspan section northeast Erbil City, Kurdistan region, Iraq

Lithostratigraphy and microfacies analysis of the Avanah Formation (Middle Eocene) were studied in the Gomaspan section in the Bina Bawi anticline, northeast of Erbil city, Kurdistan Region, Iraq. The field observations refer that the formation attains 56 m of medium to thick-bedded yellow limestone, grey dolomitic limestone, and blue marly dolomitic limestone interbedded with thin beds of blue marl and dark grey shale with an interval of sandy limestone in the middle part and thin to medium bedded limestone interbedded with red mudstone. The petrographic study of 29 thin sections of Avanah carbonates revealed that most of the matrix is carbonate mud (micrite) with few microspar. The skeletal grains include benthic foraminifera, dasycladacean green algae, ostracods, calcispheres, pelecypods, rare planktonic foraminifera, and bryozoa, in addition to bioclasts. Non-skeletal grains encompass peloids, oncoids, intraclasts, and extraclasts with common monocrystalline quartz. Three different lithostratigraphic units were identified based on field observation and petrographic analysis. They are in ascending order: A-Thick bedded dolomitic marly limestone interbedded with shale. B-Bedded dolomitic limestone interbedded with shale and marl. C-Thin to medium bedded limestone interbedded with red mudstone. Depending on detailed microfacies analysis of carbonate rocks, three main microfacies and 12 submicrofacies are recognized. From the sum of all petrographic, facies, and textural analyses, it is concluded that Avanah Formation in the Gomaspan section was deposited in the shallow marine environment, semi-restricted lagoon, in lower and upper parts, and open lagoon environment in the middle part interval.

Automated summary

Lithostratigraphy and microfacies analysis of the Avanah Formation (Middle Eocene) were studied in the Gomaspan section in the Bina Bawi anticline, northeast of Erbil city, Kurdistan Region, Iraq. The formation consists of medium to thick-bedded yellow limestone, grey dolomitic limestone, and blue marly dolomitic limestone interbedded with thin beds of blue marl and dark grey shale with an interval of sandy limestone in the middle part and thin to medium bedded limestone interbedded with red mudstone. The petrographic study revealed that the matrix is mainly carbonate mud with few microspar, and the skeletal grains include various organisms. Based on field observation and petrographic analysis, three lithostratigraphic units and three main microfacies were identified.