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we can call it an igneous rock because it coming from partial melting of preexisting rocks
Granitic magma forms at relatively shallow depths, typically between 1 and 10 kilometers beneath the Earth's surface. This type of magma is formed through the partial melting of continental crust, which is composed mainly of granitic rocks.
Normally, extrusive igneous rocks exhibit an aphanitic texture. Examples would be basalt and rhyolite.
Igneous rocks, such as granite, when subjected to extreme pressure and temperature will change to metamorphic rock. Evidence that an igneous rock had undergone metamorphism would include light and dark mineral banding; possibly with indications of partial melting in highly metamorphosed samples.
Nope, because they are created when the Earth pressurizes and heats it (but not to the point of melting). Igneous rocks are created when rocks melt.
The addition of water can lower partial melting temperatures in silicate rocks.
partial melting of mantle rocks
I have a study guide that gave this answer: All inner planets exhibit an iron-nickel core surrounded by silicate rocks.
Igneous rocks are formed in and around volcanos, metamorphic rocks are formed by the partial melting of rocks deep underground.
Magma is the result of partial melting of crustal rocks. It is a eutectic melt product.
we can call it an igneous rock because it coming from partial melting of preexisting rocks
Yes, Read A Book next time
Magma is the result of partial melting of crustal rocks. It is a eutectic melt product.
A METAMORPHIC rock is formed from other rocks that have undergone heat and pressure and partial but NOT entire melting. That is why a metamorphic rock could have layers that are distorted.
Granitic magma forms at relatively shallow depths, typically between 1 and 10 kilometers beneath the Earth's surface. This type of magma is formed through the partial melting of continental crust, which is composed mainly of granitic rocks.
What rocks contain crystals?
Normally, extrusive igneous rocks exhibit an aphanitic texture. Examples would be basalt and rhyolite.