Sandstone copper, shale-hosted copper, redbed Cu, continental redbed, Kupferschiefer type, marine paralic type, reduced facies Cu, Revett Cu. DESCRIPTION Sediment-hosted copper deposits are stratabound, that is, they are restricted to a narrow range of layers within a sedimentary sequence but do not necessarily follow sedimentary bedding. They are epigenetic and diagenetic, that is, they are formed after the host sediment is deposited, but in most cases, prior to lithification of the host. They form independently of igneous processes.