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A comparison of (super 10) Be, (super 26) Al, (super 36) Cl in boulders from a Younger Dryas moraine, Julier Pass, Graubuenden, Switzerland.
Keywords
Graubunden Switzerland;Julier Pass;boulders;moraines;upper Weichselian;Weichselian;Younger Dryas;Central Europe;Switzerland;Be 10;Al 26;chlorine;Cl 36;halogens;alkaline earth metals;beryllium;metals;aluminum;exposure age;Pleistocene;upper Pleistocene;Europe;sediments;Cenozoic;Quaternary;clastic sediments;geochronology;isotopes;radioactive isotopes