The general formula, (where A and B are metals), represent a family of phases isostructural to the mineral pyrochlore. Pyrochlores are an important class of materials in diverse technological applications such as luminescence, ionic conductivity, nuclear waste immobilization, high-temperature thermal barrier coatings, automobile
exhaust gas control, catalysts, solid oxide fuel cell, ionic/electrical conductors etc. The mineral is associated with the
metasomatic end stages of magmatic intrusions. Pyrochlore crystals are usually well-formed (euhedral), occurring usually as
octahedra of a yellowish or brownish color and
resinous luster. It is commonly
metamict due to radiation damage from included radioactive elements. Pyrochlore occurs in
pegmatites associated with
nepheline syenites and other alkalic rocks. It is also found in
granite pegmatites and
greisens. It is characteristically found in
carbonatites. Associated minerals include
zircon,
aegirine,
apatite,
perovskite and
columbite. Pyrochlore ore typically contains greater than 0.05% of naturally occurring radioactive
uranium and
thorium.
Lueshe in
North Kivu, Democratic Republic of Congo, has substantial deposits of pyrochlore. ==Crystal structure==