i dont know, but i think so.
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The two main groups of metamorphic rocks are foliated and non-foliated. Foliated metamorphic rocks show layering and parallel alignment of flat mineral crystals (ex. micas). The "banded texture in metamorphic rocks" is one of the specific kinds of foliated textures. It is referred to as gneissic banding. Essentially, this texture displays alternating layers of light and dark minerals. These rocks are called gneiss- the light bands form from quartz and feldspars, while the dark ones form from ferromagnesian minerals.
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No. The layering or foliation only occurs when there is a variation in the composition of the original rock. If the rock is homogeneous, then there will be no foliation.
No. Non-foliated metamorphic rocks include quartzite and marble.
Foliation in rocks refers to the process being split into thin sheets. It is caused by intense pressure that shapes rocks to align in particular directions.
Metamorphic rocks that do not exhibit foliation.
No, sedimentary rocks are not classified as foliated. Foliation is a textural feature found in certain types of metamorphic rocks where minerals are aligned in layers or bands due to pressure and heat. Sedimentary rocks are formed by the accumulation and cementation of sediments and do not exhibit foliation.
Foliation is a characteristic of some metamorphic rocks.
Metamorphic rocks often have foliation, which is a layered structure that results from the alignment of mineral grains due to heat and pressure during formation. Common types of foliated rocks include slate, schist, and gneiss.
Usually along the plane of foliation.
Foliation occurs deep underground.
The thin flat layering found in most metamorphic rocks is called foliation, and it is formed due to the alignment of mineral grains or the presence of alternating layers of different mineral compositions. Foliation is a common feature in rocks that have undergone high pressure and temperature conditions, leading to the development of a layered structure.
Yes, foliation is caused by directed pressure in rocks. This pressure aligns minerals in the rock, resulting in a layered or banded appearance. Foliation is common in metamorphic rocks and is a result of the rocks being subjected to deformation under pressure.
Foliation is the arrangement of minerals in a rock that results in a layered or banded appearance. It is commonly formed in metamorphic rocks through processes like pressure and temperature causing mineral alignment. Foliation is a key characteristic used to classify and identify different types of metamorphic rocks.