Mustone is a clastic sedimentary rock, not a mineral.
shale or mudstone
no not all of them for example like Bituminous coal or coal, is form by plant remains
Yes, however, those crystals are extremely small; some too small to be seen even by a microscope.
Yes, that is exactly what happens:limestone metamorphoses to marblemudstone and shale metamorphose to slatebituminous coal metamorphoses to anthracite coaletc.
yes it is a mineral
Mudstone is a clasitc sedimentary rock.
Mudstone can be changed into a metamorphic rock through the process of metamorphism, where it is subjected to high temperature and pressure. This causes recrystallization of minerals, reorganization of grains, and the development of new mineral assemblages, transforming the mudstone into a new metamorphic rock such as slate, schist, or gneiss.
Mudstone is sedimentary
Phyllite is a type of metamorphic rock, not a mineral. It is formed from the metamorphism of shale or mudstone and has a fine-grained texture with a silky sheen due to the alignment of its minerals.
Mudstone is a clastic sedimentary rock.
Mudstone is a mudrock. It is made of clay minerals and other very small pieces of rock. Mudstone is sedimentary.
Oil shale has a fine-grained texture, similar to mudstone or siltstone. It is composed of a mixture of organic matter, clay, and mineral grains.
mudstone has smaller particles :D
Another name for shale is mudstone
Slate is metamorphosed shale or mudstone.
If mudstone is subjected to high temperature and pressure over geological time, it can ultimately metamorphose into schist or gneiss, depending on the specific conditions and mineral composition. Schist typically forms under moderate to high-grade metamorphic conditions, while gneiss represents a higher grade of metamorphism with pronounced banding and foliation. Both are examples of metamorphic rocks derived from mudstone.
Examples of fine-grained rocks include shale, mudstone, siltstone, and some varieties of basalt. These rocks have small mineral grains that are not easily visible to the naked eye and typically form in environments with slow cooling or deposition rates.