IORDYE JULIET TERHEMBA2023-09-222023-09-222008-03-01https://teras.ng/api/asset/document/d675b60a-0fd1-4ab2-82cb-d94cf564f2efhttps://teras.ng/catalog-item/a2fbdff0-5803-4cf0-9a65-4851a1cd0582http://dspace.teras-network.net:4000/handle/123456789/43726Sixteen veins and other locations were mapped on the Gombe Inlier. Samples were collected and taken to the laboratory for analysis. X-Ray Fluorescence (XRF) analysis was the method employed in order to ascertain the accuracy and reliability of the results. Out of the sixteen veins analyzed, six veins were found to contain mostly Barite (BaS04), four veins were found to contain mostly Anhydrite (CaS04), while six other veins contain mainly Silica (Si02).GEOLOGY, GEOCHEMISTRY AND THE STRUCTURAL CONTROL OF BARlTE-ANHYDRJTE MlNERALIZATIONS lN THE COMBE INLIERUndergraduate Theses