Basically, silicate is (SiO2)n.SiO32- so the other element is Oxygen
(remark: compare silicate with carbonate CO32- )
Oxygen combines with silicon to form the tetrahedral structure of silicate minerals. Each silicon atom is bonded to four oxygen atoms, creating a tetrahedral unit.
Silicon combines with oxygen to form a tetrahedral structure in the mineral known as silicon dioxide, or quartz.
One example is oxygen. Oxygen combines with silicon to form silicon dioxide, SiO2.
Silicon is found in most minerals.
Silicon is abundant in the Earth's crust and combines with oxygen to form rocks and minerals, such as quartz and feldspar.
Gold is an element and as it does not contain any silicon it is therefore a non silicate.
Silicon
Platinum is a non-silicate mineral. It is classified as a native element, meaning it is composed of only one type of atom and does not contain silicate structures. Unlike silicate minerals, which are based on silicon-oxygen tetrahedra, platinum occurs in its pure metallic form and does not form silicate compounds.
The silicon-oxygen tetrahedron is the building block of silicate minerals. The word "silicate" means the compound contains silicon in some form.
Silicon is a naturally occurring element and is commonly found in the Earth's crust in the form of silicon dioxide, which is also known as silica. Therefore, silicon can be found in various states around the world, including in the form of sand, quartz, and silicate minerals.
Oxygen combines with silicon to form a tetrahedral structure in silicon dioxide (SiO2) known as quartz. Each silicon atom is surrounded by four oxygen atoms arranged in a tetrahedral shape.
Silicon is found in abundance in the Earth's crust, primarily in the form of silica and silicate minerals. It is also found in sand, quartz, and various rocks. Silicon is the second most abundant element in the Earth's crust after oxygen.