A mineral structure refers to the orderly spatial arrangement of atoms in its molecular structure. There are 14 basic arrangements of atoms in three dimensions, and all mineral structure recognised till now fit in one of these 14 arrangements.
Chemistry and structure define together a mineral. In fact, two or more minerals may have the same chemical composition, but different structures (these are known as polymorphs). For example, pyrite and marcassite[?] are both iron sulfide. Similarly, some minerals have different chemical compositions, but the same structure : for example, quartz (made from silicon and oxygen) and berlinite[?] (aluminium and phosphorous).
Minerals must be distinguished from rocks. A mineral is a chemical compound with a given composition and a defined atomic structure. A rock is a mixture of one or several minerals, in varying proportions.
There are about 3000 different mineral species known, and classifying them can range from simple (for a couple of hundred) to very difficult. A mineral can be identified by several physical properties, some of them being sufficient for full identification without equivocation. In other cases, minerals can only be classified by more complex analyses including some modern techniques such as chemical analysis and X-ray diffraction, which however, can be costly, time-consuming, and even risk damaging the sample.
Physical properties commonly used are :
silicates, which are composed largely of silicon and oxygen, with the addition of ions such as magnesium, iron and calcium. Some important rock-forming silicates include the feldspars, quartz, olivines, pyroxenes, garnets and micas.
carbonates consist of those minerals containing the anion (CO3)2- and include calcite and aragonite (both calcium carbonate), dolomite (magnesium/calcium carbonate) and siderite[?] (iron carbonate). Carbonates are commonly deposited in marine settings when the shells of dead planktonic life settle and accumulate on the sea floor. Carbonates are also found in evaporitic settings (e.g. the Great Salt Lake, Utah) and also in karst regions, where the dissolution and reprecipitation of carbonates leads to the formation of caves, stalactites and stalagmites.
Sulfates all contain the sulfate cation, in the form SO4. Sulfates commonly form in evaporitic settings where highly saline waters slowly evaporate, allowing the formation of both sulfates and halides (q.v.) at the water-sediment interface. Common sulfates include anhydrite[?] (calcium sulfate) and gypsum (hydrated calcium sulfate).
halides are the group of minerals forming the natural salts and include fluoride, common salt (known as halite[?]) and sal ammoniac[?] (ammonium chloride). Halides, like sulfates, are commonly found in evaporitic settings such as playa lakes[?] and landlocked seas (e.g. the Red Sea).
Oxides are extremely important in mining as they form the ores from which valuable metals can be extracted. They thus commonly occur as precipitates close to the Earth's surface. Common oxides include haematite (iron oxide = rust), spinel (magnesium aluminium oxide - a common component of the mantle) and ice (hydrogen oxide!).
sulfides[?] are also economically important as metal ores. Common sulfides include chalcopyrite (copper iron sulfide) and galena (lead sulfide).
phosphate group actually includes any mineral with a tetrahedral unit AO4 where A can be phosphorus, antimony, arsenic or vanadium. By far the most common phosphate is apatite which is an important biological mineral found in teeth and bones of many animals.
Some of these are scientific minerals as salt; others are elements, as potassium, calcium, iron, zinc, magnesium, copper.
These can be naturally occurring in food or added in elemental or mineral form to food, as calcium carbonate, iron fillings, etc.
Some of these additives are from natural sources as ground oyster shells for calcium carbonate.
Sometimes minerals are added to the diet separately from food, as vitamin and mineral supplements and in dirt eating, called pica or geophagy.