Red coloured Middle Eocene Gercus Formation is a widely exposed rock unit in northern Iraq, southeastern Turkey, and northwestern Iran. Siliciclastic rocks (mudstones and sandstones) are the predominant rocks of this formation which were studied petrographically and geochemically. The Gercus Formation also contains a few beds of limestone, gypsum, and conglomerate. The sandstones are of two types, red and white, mostly immature litharenites, consisting of lithics (85%), quartz (12%), and feldspars (3%). The rock fragments consist dominantly of angular chert and rounded limestone and smaller amounts of sedimentary, magmatic, volcanic, and metamorphic lithics indicating proximity of their source rocks. The provenance discrimination diagrams of the detrital grain counts in sandstones show recycled and collision orogen sources. Petrographic, heavy minerals and major and immobile trace element (e.g. La, Th, Sc, Zr, Hf, and Ti) discrimination diagrams indicated that the Gercus Formation was originated under a collision tectonic setting above a subduction zone as part of an Oceanic Island Arc (OIA), where its sediments were derived from mixed sources, including recycled sediments of chert-and carbonate-rich formations and igneous-metamorphic ophiolitic complexes of north to north-east Iraq and adjacent Iranian and Turkish counterparts. The results also indicated a mixed marine (lacustrine and deltaic) and non-marine (fluviatile) origin for the Gercus Formation. The red sandstones, white sandstones, and mudstones show minor differences in their major, trace, and rare-earth element (REE) contents and have generally similar Post Archean Australian Shale (PAAS)-, Upper Continental Crust (UCC)-, and CI-chondrite-normalized distribution patterns indicating their common origin. The average of elements in the siliciclastic rocks is depleted in the high-field-strength elements (HFSE), the large-ion lithophile elements (LILE), and REE; and enriched in some rock-forming elements (RFE) and mantle rock-forming elements (MRFE) (Mg, Ca, Cr, Co, Ni) and depleted in others (Si, Al, Fe, Cu, Zn, Ga) relative to PAAS and UCC; whereas, they are depleted in Fe, Mn, Mg, Co, Ni, Cu, Zn, Ga, Na, and P, and enriched in all other RFE, MRFE, LILE, HFSE, and REE compared to CI-Chondrite. The REE content of these rocks is very low (23-34 ppm) and their LREEs are enriched six times relative to HREEs. These geochemical characteristics suggest a provenance dominated by basic/ultrabasic rocks. The U/Th, V/Cr ratios and the authigenic U values show an oxic depositional environment for the studied siliciclastic rocks.

Sargelu Formation (Middle Jurassic) is characterized by a wide geographical distribution in Iraq and neighboring countries. This study includes two sections Barzewa and Warte locations in Erbil Governorate of Kurdistan region, Iraq, the organic, inorganic Geochemistry and mineralogical properties were recorded. Fifteen samples of Sargelu Formation black shales were gathered from both locations. The source rocks of the black shales have an intermediate to felsic composition. The illite crystallinity index (IC) of the studied black shale shows the high anchizone stage. The organic geochemical parameters were analyzed in Sargelu Formation, the black shale contains type II - III kerogen. The average total organic carbon (TOC) of black shale for both section is 4.29 wt.%. By using the ultrasound homogenizer process the C-H bond (hydrocarbon component) of black shale recovered from the solid state to the liquid state.

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