Syngenetic and epigenetic ore deposits represent two fundamental modes of ore formation in relation to the host rocks and geological processes. Syngenetic deposits are those that formed simultaneously with the deposition of the host rock. These deposits are often stratiform or stratabound and are closely linked with sedimentary or volcanic processes. In sedimentary environments, syngenetic deposits are commonly associated with chemical precipitation, mechanical concentration, or biological activity. For example, banded iron formations (BIFs) are classic syngenetic deposits where iron minerals such as hematite and magnetite precipitated directly from seawater along with silica during the Precambrian period. Similarly, manganese nodules, phosphate deposits, and certain types of lead-zinc ores in carbonate rocks exhibit syngenetic characteristics. Volcanogenic massive sulfide (VMS) deposits also fall under syngenetic deposits, forming on or near the seafloor due to hydrothermal activity related to submarine volcanism, where sulfide minerals precipitate contemporaneously with the volcanic rocks. Epigenetic deposits, on the other hand, form after