Geology and geochemistry of granite rocks of Kampung Sungai Mekong Jeli, Kelantan

There are two smaller units of sedimentary rocks limestone, and sandstone. The smaller units of limestone and sandstone are dated to be Permian-Triassic. The research area's geomorphology can be categorized into high hills, medium hills, and low relief morphology unit areas. Lineament features, joint structures, and fold structures are some of the principal geological structures in the studied region. For the investigation of granite rock, two granite samples the from the study area were analyzed using X-ray Fluorescence (XRF) and Inductively Coupled Plasma Mass Spectrometry (ICPMS) for major and trace elements and for rare earth elements respectively. The granite that is found in the study area is classified as S-type and shows a peraluminous characteristics as the value of A/CNK is higher than 3. As conclusion, the geological mapping of the study area and the study of petrography and geochemistry of granite rocks provides important information for geological and environmental management, mineral exploration, and economic development.