Gabbro is a type of mafic, phaneritic igneous rock.
Rock salt is neither felsic nor mafic. It is a type of sedimentary rock composed primarily of halite (or sodium chloride) minerals. Felsic and mafic are terms used to describe igneous rocks based on their silica content and mineral composition.
Granite is a phaneritic rock. Phaneritic rocks are coarse-grained, and they have visible crystals. Other phaneritic rocks include diorite, gabbro, and periodite. These rocks are also intrusive because they cool slowly.
Large size crystals that are known as phaneritic are typically found in intrusive igneous rocks. These rocks cool slowly beneath the Earth's surface, allowing the crystals time to grow to visible sizes. Phaneritic textures are characterized by crystals that are easily visible to the naked eye.
Basalt is a common example of a mafic rock. It is dark in color, fine-grained, and rich in minerals like pyroxene and olivine. Basalt is formed from the solidification of magma with low silica content, typically from volcanic activity.
Monzonite is an intermediate rock.
Yes, Gabbro is a phaneritic igneous rock.
Phaneritic refers to igneous rock grain size,which is visible with the naked eye.
Rock salt is neither felsic nor mafic. It is a type of sedimentary rock composed primarily of halite (or sodium chloride) minerals. Felsic and mafic are terms used to describe igneous rocks based on their silica content and mineral composition.
Granodiorite is a phaneritic, intrusive igneous rock composed primarily of plagioclase feldspar, quartz, and one or more mafic minerals such as biotite or hornblende. It has a composition intermediate between granite and diorite.
Texture
Granite is a phaneritic rock. Phaneritic rocks are coarse-grained, and they have visible crystals. Other phaneritic rocks include diorite, gabbro, and periodite. These rocks are also intrusive because they cool slowly.
A Mafic Extrusive Igneous Rock.
Granite rock is not porphyritic. It is phaneritic because it has a coarse-grained texture.
Chemical classification is not a compositional classification of magma. Compositional classifications include mafic, intermediate, and felsic based on the silica content of the magma.
Large size crystals that are known as phaneritic are typically found in intrusive igneous rocks. These rocks cool slowly beneath the Earth's surface, allowing the crystals time to grow to visible sizes. Phaneritic textures are characterized by crystals that are easily visible to the naked eye.
No. Granite is an intrusive felsic rock.
Amphibolite is a type of metamorphosed mafic igneous rock. It is composed largely of minerals such as hornblende and plagioclase.