

Use of chlorine-36 as tracer for the evolution of waters in geothermal and tectonic active areas in western Turkey.
Keywords
western Turkey;heat flow;tectonics;North Anatolian Fault;thermal waters;water regimes;water rock interaction;Turkey;radioactive tracers;residence time;ground water;Middle East;chlorine;Cl 36;halogens;Asia;isotopes;radioactive isotopes