The central Idaho metallogenic province hosts numerous mineral deposit types. These include Late Cretaceous precious-polymetallic vein deposits, amagmatic Paleocene-Eocene breccia-hosted gold-tungsten-antimony deposits, and Eocene mercury deposits in metasedimentary roof pendants and in Late Cretaceous granitoids. Hot-springs gold deposits in Eocene volcanic rocks are also included in the central Idaho province. New sensitive high mass-resolution ion microprobe (SHRIMP) uranium-lead (U-Pb) ages for igneous rocks and for detrital zircon analyses of metasedimentary rocks along with geologic mapping clarify the geologic framework of the mineral deposits. This framework includes (1) structural controls for regional distribution of mining districts, (2) progressive structural development of individual districts, (3) regional sedimentary facies and their control of metals associations resulting in regional belts, and (4) influences of the several regional magmatic events.Because diverse metasedimentary, plutonic, and volcanic rocks host epigenetic deposits in the central Idaho mining districts (figs. 2, 3), there is a broad range of proposed deposit origins and a common linkage to a variety of proposed mineral belts. These mineral belts have been characterized using geographic groupings or, commodities, but the belts, so defined, resulted in intersecting linear arrays of deposits (for example, Bookstrom and others, 1998). Although not ascribed to geologic causes, these include (1) northwest-striking Florence-Stibnite gold belt, (2) north-northeast-striking Dixie-Thunder Mountain gold belt, (3) northeast-striking Marshall Lake-Elk City polymetallic belt (Green, 1972), (4) northeast-striking Idaho-Montana porphyry belt (Green, 1972; Rostad and others, 1978; Armstrong and others, 1978), (5) north-northwest-striking tungsten belt (Cook, 1956), and (6) northwest-striking Idaho cobalt belt (Hughes, 1983;Hahn and Hughes, 1984). Most of these are substantially modified or abandoned by new studies and so are not shown on maps for the present study.In interpretations of their genesis, polymetallic deposits in central Idaho were initially interpreted as related to the Late