Silicates are the most abundant type of minerals in Earth, these are the result of the combination of silicon and oxygen along with other materials. Additionally, not all silicates are identical but differ in composition and physical/chemical features. Indeed, silicates are often classified as dark or dark silicates. In the case of dark silicates, these include different types of silicates such as olivine and biotite that are dark because they contain silica tetrahedral but also iron and magnesium. Thus, dark silicates are primarily composed of silica tetrahedral and iron and magnesium, which is also why they are known as ferromagnesian silicates.
The middle nitrogen has two sigma bonds and one pi bond. You know that one p orbital is used in the double bond and two sp2 orbitals are involved in the sigma bond. This leaves one sp2 orbital for the lone pair to occupy.