Mafic vs felsic mafic and felsic are categories into which igneous rocks are classified.
Is granite felsic intermediate or mafic.
Mafic felsic and intermediate extrusive rocks.
It is commonly erupted as passive lava flows due to its low viscosity.
Intermediate magmas are somewhat more viscous than the mafic magmas.
For example granite contains around 70 of silica.
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.
More general terms for these rocks are mafic felsic and intermediate.
This is an order showing increased silica content.
Felsic intermediate mafic ultramafic.
The most common felsic rock is granite which represents the purified end product of the earth s internal differentiation process.
Compilations of many rock analyses show that rhyolite and granite are felsic with an average silica content of about 72 percent.
Which of the following is an aphanitic igneous rock.
Therefore rocks are divided into ultramafic mafic intermediate and felsic.
Felsic rocks are mostly feldspar especially k feldspar at least 10 quartz and less than 15 mafic minerals biotite hornblende.
Mafic rocks have between 45 and 55 of silica whereas felsic rocks have over 65 of silica the highest of all types.
Gabbro and basalt are mafic with an average silica content of 48 percent.
Part i volcanic extrusive rocks.
Syenite diorite and monzonite are intermediate with an average silica content of 59 percent.
Mafic rocks have about 50 percent silica and high amounts of iron magnesium and calcium and are dark in color.
Basalt is an extrusive mafic volcanic rock.
Felsic rocks are composed of high levels of magma silicate materials and rocks which are also rich in potassium oxygen silicon and sodium.
A common mafic rock is basalt.
Intermediate rocks are roughly even mixtures of felsic minerals mainly plagioclase and mafic minerals mainly hornblende pyroxene and or biotite.
There is little or no quartz.
All felsic rocks contain a high percentage of silica.
Diorite is the name given to intrusive intermediate rocks whereas andesite is the name given to extrusive intermediate rocks.
Granite is a great example of felsic rocks and muscovite quartz and some feldspar are the best examples of felsic minerals.
Whereas magma mixing occurs when two ascending bodies of magma join and mix together into a composition that is intermediate to the two original magmas.
Granite is a felsic rock.
And peridotite is an ultramafic rock with an.
Due to the color of the minerals forming them the rocks are either light or dark.