There are two answers to this question1) gneissic
for bands in such as granitic gneiss
2) foliated for thin layers seen in schist.
Metamorphic rock with mineral grains arranaged in bands or lamellar planes are called foliated metamorphic rocks.
Metamorphic rock with mineral grains arranaged in bands or lamellar planes are called foliated metamorphic rocks.
Metamorphic rock with mineral grains arranaged in bands or lamellar planes are called foliated metamorphic rocks.
What kind of metamorphic rock has its mineral grains arranged in planes or bands
Foliated rock. If you are looking for whether the rock has no bands it is non-foliated.-Anonymous person but very smart ! :)
No, foliated metamorphic rocks have mineral grains that are aligned in parallel layers or bands due to the pressure and temperature conditions during their formation. This alignment gives foliated rocks their characteristic layered appearance.
Metamorphic rocks such as marble and quartzite are said to be non-foliated because their mineral grains are not arranged in parallel layers or bands like in foliated rocks such as slate or schist. This lack of alignment gives non-foliated rocks a more uniform texture and appearance.
The banding of metamorphic rock, specifically gneiss, results from the segregation of dark and light mineral grains. This occurs due to high-grade metamorphic processes, where intense heat and pressure cause the original minerals to recrystallize and align, creating distinct bands of differing mineral compositions. The lighter bands typically consist of quartz and feldspar, while the darker bands contain biotite, amphibole, or other ferromagnesian minerals. This characteristic banding gives gneiss its striking appearance and is a key feature in identifying the rock.
The type of rock that forms when crystals combine and create visible bands is called metamorphic rock, specifically a foliated metamorphic rock. An example of this is gneiss, which features alternating layers of different mineral compositions. The banding occurs due to the alignment of mineral grains under pressure and temperature conditions.
grains arranged in solid bands.
The parallel arrangement of mineral grains in a rock that gives it a striped appearance is called foliation. This typically occurs in metamorphic rocks due to the alignment of minerals under pressure and heat, resulting in distinct bands or stripes. Foliation can provide clues about the rock's history and the direction of metamorphic forces.
Rock