Petrography study of the recent sediments in Hareer’s region at Basrah Governorate - Southern Iraq

• Published in: IOP conference series. Earth and environmental science 2024-02, Vol.1300 (1), p.12014
• Main Authors: Al-Sudani, K J, Albadran, B N, Al-hadadi, A S Y, Al-Jaberi, M H, Pournelle, J R
• Format: Article
• Language: English
• Subjects: Basrah Governorate; Biotite; Chert; Clay minerals; Hareer’s region; Heavy and Light Minerals; Hematite; Iron oxides; Kyanite; Limonite; Mica; Minerals; Muscovite; Oxidation; Oxidation process; Petrography; Quartz; Sedimentary basins; Sedimentary rocks; Sediments; Tourmaline; Zircon
• ISSN: 1755-1307; 1755-1315
• DOI: 10.1088/1755-1315/1300/1/012014

Two sites of Hareer’s region is located in the southern part of Iraq, specifically in the northern Basrah Governorate. The sites are at a depth of 5 meters. The results of heavy mineral analysis showed that there are fifteen types include; Opaque grain (Iron Oxide), Chlorite, Muscovite mica, Biotite, Orthopyroxene, Clinopyroxene, Amphibole (Hornblende and Actinolite), Epidote, Garnet, Kyanite, Staurolite, Zircon, and Tourmaline. On the other hand the light minerals and the results of the mineral analyses revealed that they were primarily composed of rock fragments, with a variety of quartz minerals, feldspar minerals, evaporate minerals, clay-coated grains, and trace amounts of unidentified minerals. The abundance and diversity of heavy minerals indicate the diversity of the sources of the parent rocks, such as igneous, metamorphic and sedimentary rocks. The large amount of opaque and small amount of other minerals in the study area samples is due to the oxidation process where many of the ferromagnesian minerals such as pyroxenes, and hornblende decompose to form iron oxides (e.g. hematite, limonite). Light minerals were visible as irregular, sharp, or occasionally semi-sharp crystalline forms, which suggests that the sources were close by and that the light minerals originated from the sedimentary basin or within it through the processes of deposit erosion and re-deposition. The study area, which is a part of the Undissected Arc, is primarily distinguished by a high content of quartz (mono- and polycrystalline quartz, including chert), and feldspar, which can occur in fluvial environments.