silicates- silicon and oxygen
carbonates- carbon, oxygen, and 1 or more other elements
oxides- oxygen and 1 or more other elements( usually metal)
sufates/sulfides- contain sulfur
halides- halogen ion and 1 or more other elements
native elements- group of minerals that exists in relatively pure form( ex: gold, silver, copper, sulfer, carbon...)
In Bowen's reaction series, feldspar minerals go through a continuous change of composition, while iron-magnesium groups have an abrupt change of mineral types. When magma cools, the feldspars that form are calcium-rich. As cooling continues, the feldspars react with magma and the feldspar composition changes. The result is a zoned crystal with sodium-rich outer layers and calcium-rich core. For iron-magnesium minerals, when magma starts cooling, a mineral begins to crystallize. However, when the magma temperature drops, a whole new mineral begins to form. The previously formed minerals reacts with the magma and is converted into the new mineral.
industrial minerals or building materials
The grouping of silicate and non-silicate minerals is based on whether they contain silicon and oxygen. Silicate minerals are divided into smaller groups based on their structure. Non-silicate minerals are didvided into smaller groups based on their composition.
oxygen 46.6%
Minerals and groups of minerals can be classified as an ore when they contain a sufficient amount of desired material, most times metals, to be extracted and processed feasibly.
Minerals are grouped by their chemical composition. There are more than 3 groups of minerals including. Silicates, oxides, sulfates, sulfides, carbonates, native elements, and halides are all major mineral groups. Silicates are definitely at the top of the list.
mineral is a naturally occurring solid chemical substance formed through biogeochemical processes, having characteristic chemical composition, highly ordered atomic structure, and specific physical properties. By comparison, a rock is an aggregate of minerals and/or mineraloids and does not have a specific chemical composition. Minerals range in composition from pure elements and simple salts to very complex silicates with thousands of known forms.[1] The study of minerals is called mineralogy.Contents[hide] 1 Mineral definition and classification2 Crystal structure 2.1 Mineral groups and solid solution3 Differences between minerals and rocks 3.1 Mineral composition of rocks4 Physical properties of minerals5 Chemical properties of minerals 5.1 Silicate class5.2 Carbonate class5.3 Sulfate class5.4 Halide class5.5 Oxide class5.6 Sulfide class5.7 Phosphate class5.8 Element class5.9 Organic class6 See also7 References8 External links
Silicates Minerals. Eg. Quartz (SiO2).
industrial minerals or building materials
In Bowen's reaction series, feldspar minerals go through a continuous change of composition, while iron-magnesium groups have an abrupt change of mineral types. When magma cools, the feldspars that form are calcium-rich. As cooling continues, the feldspars react with magma and the feldspar composition changes. The result is a zoned crystal with sodium-rich outer layers and calcium-rich core. For iron-magnesium minerals, when magma starts cooling, a mineral begins to crystallize. However, when the magma temperature drops, a whole new mineral begins to form. The previously formed minerals reacts with the magma and is converted into the new mineral.
The two basic groups of metallic mineral resources are ferrous minerals, which contain iron, and non-ferrous minerals, which do not contain iron. Ferrous minerals include iron ore, while non-ferrous minerals include copper, lead, zinc, gold, and silver.
There are over four thousand different minerals. There are some major groups of minerals, which include groups such as oxides, silicates, carbonates, phosphates, borates, halides, sulfides, and native elements.
The grouping of silicate and non-silicate minerals is based on whether they contain silicon and oxygen. Silicate minerals are divided into smaller groups based on their structure. Non-silicate minerals are didvided into smaller groups based on their composition.
Minerals are classified as oxides, sulfides, halides, sulfates, silicates, or carbonates. Some elements are also classified as minerals. There's also a metallic and non-metallic mineral classification.
oxygen 46.6%
oxygen 46.6%
oxygen 46.6%