Hydrocarbons have been found in intrusive and metamorphic rocks, such as granite, in regions like Vietnam and Venezuela. This phenomenon is often attributed to the migration of oil from sedimentary source rocks into these igneous formations, rather than from other reservoirs. The presence of hydrocarbons in igneous rocks is not common but has been documented for over 75 years, with various studies highlighting occurrences globally. In some cases, hydrocarbons can be trapped in fractured granite or associated with granite wash, which consists of eroded material from granite. The migration of oil can occur through structural features like unconformities, brittle faulting, or shear zones that allow hydrocarbons to move from deeper sedimentary layers into the overlying igneous rocks. Additionally, some theories suggest that hydrocarbons may originate from deeper mantle sources or through biological processes involving extremophiles.