Common Mafic Rocks Are Granit

Learn more about the properties and uses of granite in this article.

Common mafic rocks are granit.

Many of the lunar rocks brought back to earth through the apollo missions are classified as gabbro with high amounts of olivine and other mafic minerals. All are produced by partial melting of the uppermost asthenosphere. Felsic and mafic rocks division of igneous rocks on the basis of their silica content. It is relating to denoting or containing a group of dark colored mainly ferromagnetic minerals such as pyroxene and olivine.

Granite coarse or medium grained intrusive igneous rock that is rich in quartz and feldspar. Granite ˈ ɡ r æ n ɪ t is a common type of felsic intrusive igneous rock that is granular and phaneritic in texture. Peridotite is a common rock found in the deeper mantle of the earth and exhibits more olivine and less quartz than gabbro although both are considered mafic igneous rocks. Mafic rocks are dark in color.

Strictly speaking granite is an. Granites can be predominantly white pink or gray in color depending on their mineralogy the word granite comes from the latin granum a grain in reference to the coarse grained structure of such a completely crystalline rock. The most common felsic rock is granite which represents the purified end product of the earth s internal differentiation process. Felsic magma or lava is higher in viscosity than mafic magma lava.

Because of their relatively low viscosity mafic lavas may travel great distances and flood the landscapes over which they flow. It is the most common plutonic rock of the earth s crust forming by the cooling of magma silicate melt at depth. The most common felsic rock is granite. Chemical analyses of the most abundant components in rocks usually are presented as oxides of the elements.

Mafic lava flows are thin and sometimes called plateau or flood lavas. It is important to note that there are many intermediate steps in the purification process and many intermediate magmas which are produced during the conversion from mafic to felsic. Common felsic minerals include quartz muscovite orthoclase and the sodium rich plagioclase feldspars albite rich. Common mafic rocks include basalt dolerite and gabbro.

Igneous rocks typically consist of approximately 12 major oxides totaling over 99 percent of the rock of the oxides silica sio 2 is usually the most abundant. Granite is the most common intrusive igneous rock figure 4 4. Mafic rocks regardless of tectonic setting have one thing in common.