Mineral replacement fossils are fossils that preserve the structure of the original organically produced matter without actually preserving any of the original material.
The agatized shells mentioned above are a good example. An even better example is petrified wood, which has absolutely no wood at all in it - it has been 100% replaced with silica - but which preserves structures sometimes right down to the cellular level.
Typically these types of fossils involve silica, since silica is often deposited as a colloid and ends up forming micro-fine crystals that can preserve structures very well. Occasionally you see other replacements such as pyrite replacing what were originally shells.
•Replacement of minerals with other minerals
-Petrification
-Permineralization
Silicification of shells
stop cheating
Total replacement of the minerals: replacement fossilization. Partial replacement of the minerals: perminalization fossilization.
The replacement of organic material with minerals over a period of time, as in petrified wood, is an example of the process of mineralization.
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
Rocks and minerals
where are minerals located where thier are volcanoes or trenches
Total replacement of the minerals: replacement fossilization. Partial replacement of the minerals: perminalization fossilization.
Replacement minerals.
Replacement process is a process in which stone recieves minerals
Replacement process is a process in which stone recieves minerals
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. ~Follow me on Twitter: @jennholguinxo I follow back!
Fossils form through the process of mineral replacement beginning when an organism dies and is buried. Groundwater seeps around the organism, and the minerals in the water gradually replace the minerals in the hard parts of the organism. Over time these minerals turn into a stone replica of an organism.
It's called fossilization, and in particular, replacement and recrystallization.
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
The replacement of organic material with minerals over a period of time, as in petrified wood, is an example of the process of mineralization.
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
yes minerals can create other minerals.
Minerals are made up of well minerals. there is no other way to explain it. Minerals are Minerals.