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The Palmottu U-ore deposit, located in a granitic host rock in southern Finland, provides an excellent location for analogue studies to assess the radionuclide transport from the U-ore deposit along welldefined pathways in the fractured crystalline rock [ 1 ] . In this context, strontium and boron isotope ratios are used to trace the degree of water-rock interaction and mixing processes in groundwaters. Sr and B analyses have been performed on groundwater from the Palmottu hydrosystem and, indoi:10.1180/minmag.1998.62a.1.147 fatcat:lgeghrs2knawvkyooys67rm3qq