Pink granite would consist primarily of potassium feldspar and quartz with minor amounts of mica and other feldspars.
Orthoclase feldspar
Quartz, feldsper, biotite, muscovite.
No. Diorite has the same composition as andesite while Rhyolite has the same composition as granite.
Yes. Granite and Rhyolite have the same composition.
Magma forms coarse crystalline intrusive igneous rocks such as granite or gabbro, depending on the chemical composition of the magma.
granite has its composition _ quartz+alkali feldspar
Granite is intrusive, can be pink, and contains mica.
They are roughly the same. If they are from the same source of magma, they could be nearly identical in chemical composition.
No. Diorite has the same composition as andesite while Rhyolite has the same composition as granite.
Andesite is considered an intermediate rock between granite (felsic igneous rock) and basalt (mafic igneous rock), based on chemical composition.
The difference is the size of grains. Rhyolite is the felsic igneous rock with fine-grained size. Whereas, granite is the equivalent in composition but with coarse-grained size.
Intrusive: Extrusive Equivalent Granite: Rhyolite Diorite: Andesite Gabbro: Basalt
who cares
It contains about 70% Silica(SiO2)Added:Rhyolite, a gost town town in South-Nevada, is named for rhyolite, an igneous rock composed of light-colored silicates, usually buff to pink and occasionally light gray. It belongs to the same rock class, felsic, as granite but is much less common.
Rocks have a composition between that of granite and basalt
Yes. Granite and Rhyolite have the same composition.
Magma that is high in silica usually forms light-colored rock, such as granite. Grantis, however, comes in many shades and colors, from nearly black to light gray, red, and pink. The mineral composition of granite determines its color. ^______^
How are basalt and granite diffrerent in their origin texture and mineral composition How are the similar
Magma forms coarse crystalline intrusive igneous rocks such as granite or gabbro, depending on the chemical composition of the magma.