文摘
The Ravar copper belt (RCB) was introduced for first time. The RCB is a Cu-Ag-U red bed type sediment-hosted stratiform copper (SSC) belt. Spionkopite as a common supergene mineral in the SSC deposits, is recognized in this belt. Marcasite that was less reported in SSC deposits of the world, is a common mineral in the RCB.