silicates
Silicate minerals are those composed of silicon and oxygen atoms. Some of these minerals are quartz, feldspar, mica and olivine.
silicates
Most of the rocks contain Silicates as the basic material, silicates are anions containing Silicon and oxygen and in combination with metallic cations mostly Calcium and Magnesium. These are the basics, but there are hundreds of different kinds.
The earth's mantle is not made of metal but is a mixture of many somewhat molten rocks, most as oxides, meaning the mantle may be more oxygen than metal. The metals it has the most of are magnesium, iron, and aluminum. There's also lots of silicon, which is not really a metal.
no
Igneous rocks are mostly made up of silicate minerals. These silicates are of two types, light and dark silicates. The dark silicates are also called ferromagnesian because of the presence of iron and magnesium in them. They include olivine, pyroxene, amphibole and biotite. The light-colored silicates include quartz, muscovite and feldspar. You can learn more about igneous rocks when you check the link.
silicates
Ores.
Most of the rocks contain Silicates as the basic material, silicates are anions containing Silicon and oxygen and in combination with metallic cations mostly Calcium and Magnesium.
Silicates. The largest and most important mineral family consists of the silicates. The bulk of rocks of the crust are composed of silicate materials, which combine the two most abundant chemical elements in the lithosphere, oxygen and silicon.
The largest group of minerals by far are the silicates (most rocks are ≥95% silicates), which are composed largely of silicon and oxygen , with the addition of ions such as aluminum, magnesium, iron, and calcium. Some important rock-forming silicates include the feldspars, quartz, olivines, pyroxines, amphiboles, garnets, and micas.
17%
silicates
Silicate minerals are those composed of silicon and oxygen atoms. Some of these minerals are quartz, feldspar, mica and olivine.
It's safe to say most rocks are chemically silicates, although the commonest rocks contain oxides of calcium, magnesium, and other metals. Recent discoveries indicate the most common rock inside the Earth is a magnesium-iron-silicate, although it is difficult to obtain.
Lee C. Peck has written: 'Systematicanalysis of silicates' -- subject(s): Geochemistry, Analysis, Silicates, Rocks