Despite the abundance of silicons in the Earth's crust, not all minerals contain silicon. The atoms of many metals, which tend to lose electrons and become positively charged, like to bond with other atoms or groups of atoms that tend to gain atoms and become negatively charged. For example, atoms of sodium, a metal, and chlorine, a non-metal, pair up in equal numbers to form sodium chloride, also known as halite (or common table salt). Other important types of non-silicate minerals include carbonates, with metals bonded to groups of carbon and oxygen atoms; oxides, with metals joined to oxygen alone; sulfides, which consist of metal and sulfur atoms; and sulfates, in which groups of sulfur and oxygen atoms are joined with metal atoms.