Uranium deposits occur in the Olden granite of approx 1650 m.y. in age. This granite outcrops in the northern and eastern segments of the Precambrian Olden window of the central Swedish Caledonides. The Olden granite is a 'highly evolved' biotite granite, with SiO2 >70%. The granite was rich in U (and other incompatible trace elements) and much of the U was located in labile sites. During the Caledonian orogeny 420 m.y. ago, the granite was metamorphosed to greenschist facies, clastically deformed, hydrothermally altered in turn, and mineralized along fractures with quartz, fluorite, calcite and galena. Pitchblende and coffinite were locally deposited as fracture fillings, in particular association with biotitic alteration, whose relation to hydrothermal alteration is obscure; biotite is concentrated along fractures. The U deposits are partly and 'recently' oxidized. The Pb-U, Pb-Pb, and Sr-Rb isotopic systems of most samples were strongly to completely reset by the Caledonian orogeny. The source and host of the Lilljuthatten uranium ore was a special type of granite. The granite fractured, U was mobilized by metamorphism, and deposited in the fractures, and the deposit was preserved from weathering. Similar U deposits in high U granites, common in the Swedish Caledonides, should occur elsewhere.-G.J.N.