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Yes diorite's texture is aphanitic.
Rhyolite may be aphanitic or porphyritic.
A phaneritic texture.
Texture
It is not true. Most crystallized (solidified, cooled) lava produces rock with an aphanitic texture (mineral grains too small to be seen without magnification).
Phaneritic rock has visible identifiable crystal grains. Aphanitic rock has crystal grains that are too small to be visible with the naked eye. In igneous rock, the difference is due to the amount of time spent in cooling. Long term cooling of magma underground leads to large crystals, rapid cooling of lava above ground leads to small crystal texture.
And their texture, which can be aphanitic, phaneritic, glassy, or porphyritic. mineral composition and crystal texture
Yes diorite's texture is aphanitic.
Rhyolite may be aphanitic or porphyritic.
A phaneritic texture.
The display a phaneritic texture.
Texture
It is not true. Most crystallized (solidified, cooled) lava produces rock with an aphanitic texture (mineral grains too small to be seen without magnification).
Texture: Aphanitic -- small crystals, invisible without magnification Porphyritic -- visible crystals amid a fine-grained groundmass Phaneritic -- large visible crystals Composition: Felsic -- more than 65% silica Intermediate -- between 55-65% silica Mafic -- between 45-55% silica Ultramafic -- less than 45% silica
A rock with large crystals indicates that the rock cooled slowly. It is referred to as a phaneritic texture when a rock forms this way.
Phaneritic is the texture of igneous rocks. These types of rocks crystallized slowly.
phaneritic