Foliation
Large mineral crystals that are all about the same size are formed from magma that cooled slowly inside the earth. Small mineral crystals (not identifiable without a microscope) formed from magma that cooled rapidly, on or near the surface of the earth.
One of the two ways that parent rock affect the metamorphic process is through the mineral makeup. Another factor is chemical composition.
The major factor is the amount of time the magma remains mostly liquid while cooling and solidifying. More time spent cooling produces larger crystals because of the free movement of a mineral's constituent isotopes in a somewhat liquid magma.
When igneous rocks cool quickly, they have small crystals and have a texture that may be described as aphanitic. When igneous rocks cool slowly, they have much larger crystals and have a texture that may be described as phaneritic or pegmatitic.
Usually, the determining factor is the size of the mineral crystals in the rock. Igneous rocks that have solidified above ground cool quickly and have less time for larger crystals to grow.
Large mineral crystals that are all about the same size are formed from magma that cooled slowly inside the earth. Small mineral crystals (not identifiable without a microscope) formed from magma that cooled rapidly, on or near the surface of the earth.
evaporation
fluoresence is not a factor. I had this same question and i got fluorescence as a correct answer
fluoresence is not a factor. I had this same question and i got fluorescence as a correct answer
One of the two ways that parent rock affect the metamorphic process is through the mineral makeup. Another factor is chemical composition.
The main factor is time spent in cooling and solidifying. More time means larger crystals.
The major factor is the amount of time the magma remains mostly liquid while cooling and solidifying. More time spent cooling produces larger crystals because of the free movement of a mineral's constituent isotopes in a somewhat liquid magma.
Temperature doesn't really affect the crystal size; the rate of cooling is the major factor. The faster the mineral, rock, etc. (whatever has the crystals) cools, the smaller the crystals- the slower the larger. If you were "growing" crystals with a set, the warmer the temperature generally means the larger the crystals.
When igneous rocks cool quickly, they have small crystals and have a texture that may be described as aphanitic. When igneous rocks cool slowly, they have much larger crystals and have a texture that may be described as phaneritic or pegmatitic.
can color be a denitive factor in determinig a mineral
Usually, the determining factor is the size of the mineral crystals in the rock. Igneous rocks that have solidified above ground cool quickly and have less time for larger crystals to grow.
Crystal size in igneous rock is predominately a factor of time spent in cooling from lava or magma. Samples with relatively large crystals are the result of the magma having spent a longer amount of time at ideal crystal forming temperatures for each mineral present.