Ásványosodási
Ásványosodási refers to the geological process by which organic matter is transformed into mineral matter. This occurs over extended periods through the interaction of geological agents and the original organic material. Typically, this process involves the replacement of the organic components with inorganic minerals. The original structure and form of the organic material can sometimes be preserved, resulting in fossils.
Several factors contribute to ásványosodási. The presence of mineral-rich groundwater is crucial, as it carries dissolved
Common examples of ásványosodási include petrified wood, where the cellulose and lignin of wood are replaced