Minerals such as silca, iron, and pyrite are critical for fossilization in both processes. However, in replacement, the hard structures of the organism dissolve and are replaced with minerals. During replacement, the original microscopic details, such as the inside of a bone, are partially or totally destroyed.
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The replacement of organic material with minerals over a period of time, as in petrified wood, is an example of the process of mineralization.
Total replacement of the minerals: replacement fossilization. Partial replacement of the minerals: perminalization fossilization.
Permineralization is one of the ways in which a plant or animal can be turned into a fossil.
Permineralization is the process of fossilization where mainly water mineral deposits take the form of the organism. The minerals harden with time and pressure from over laying deposits turning into rock. Petrification happens when silica binds with celulose of a plant and turns into stone often retaining the microstructure of the plant.
Permineralized fossil are formed when dissolved minerals precipitate from a solution in the space occupied by the organism's remains.
Permineralization
In geology, petrification or petrification is the process by which organic material becomes a fossil through the replacement of the original material and the filling of the original pore spaces with minerals. So yeah the answer is petrification
permineralization
permineralization
Permineralization.
permineralization
The process is call petrification, via permineralization.